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noRm c 







jasper L. stuckey, State geologist 

Bulletin Number 49 




and Others 

Prepared by Geological Survey, U. S. Department of the Interior 

in cooperation with the 
North Carolina Department of Conservation and Development 


North Carolina 
Department of Conservation and Development 

R. Bruce Etheridge, Director 

Division of Mineral Resources 

Jasper L. Stuckey, State Geologist 

Bulletin Number 49 


J. C. Olson 
and Others 

Prepared by Geological Survey, U. S. Department of the Interior 

in cooperation with the 
North Carolina Department of Conservation and Development 



Governor R. Gregg Cherry, Chairman Raleigh 

J. L. Horne, Vice-Chairman Rocky Mount 

Charles S. Allen Durham 

Oscar P. Breece . Fayetteville 

J. Wilbur Bunn Raleigh 

K. Clyde Council Wananish 

R. Floyd Crouse Sparta 

W. J. Damtoft Canton 

Percy B. Ferebee Andrews 

A. H. Guion . Charlotte 

W. Roy Hampton Plymouth 

R. W. Proctor Marion 

Miles J. Smith Salisbury 

D. M. Stafford Pomona 

A. K. Winget Albemarle 

J. R. Wollett Littleton 

R. Bruce Etheridge, Director 




Letter of Transmittal vi 

Preface vii 

General summary, by J. C. Olson 1 

Abstract 1 

Introduction 1 

Geography 2 

•Field work and acknowledgments 4 

Previous work 4 

General geology 5 

Metamorphic rocks 5 

Weathering , 5 

Igneous rocks 5 

Coarse-grained granite 5 

Other granite bodies 5 

D unite 6 

Structure 6 

Folds 6 

Fractures 6 

Pegmatites 7 

Size and shape 7 

Structure .'. 7 

Wall-rock alteration 8 

Mineralogy 8 

Mineral distribution 9 

Quartz cores 9 

"Burr rock" 9 

Border zones 10 

Feldspathic pegmatite 10 

Granite in pegmatite 10 

Occurrences of muscovite 10 

Disseminated mica . : 11 

Mica related to quartz cores 11 

Mica related to walls 12 

Mica associated with granite bodies 13 

Source and emplacement of pegmatite 13 


CONTENTS — Continued 


Muscovite 13 

Properties 13 

Classification and grading 14 

Qualitative distribution 15 

Mining 15 

History 15 

Methods 16 

Economic factors 16 

Scrap mica : 17 

Feldspar 17 

Past production 17 

Future possibilities 19 

Descriptions of selected mines : 20 

Allman Cove mine, by J. M. Parker III 20 

Beasley No. 1 mine, by M. R. Klepper and J. C. Olson 20 

Beasley No. 2 mine, by M. R. Klepper and E. Wm. Heinrich 22 

Big Flint mine, by E. Wm. Heinrich 26 

Big Ridge mine, by M. R. Klepper and E. Wm. Heinrich 28 

Bowers mine, by D. M. Larrabee and E. Wm. Heinrich 32 

Cox mine, by W. C. Stoll 32 

Engle Cope mine, by E. Wm. Heinrich 34 

Frady mine, by D. M. Larrabee 36 

Iotla-Bradley mine, by D. M. Larrabee 37 

Kiser mine, by E. Wm. Heinrich 38 

Lyle Knob mine, by J. M. Parker III and W. C. Stoll 40 

Moody mine, by J. M. Parker III and W. C. Stoll 42 

Poll Miller mine, by E. Wm. Heinrich 42 

Rocky Face Knob mines, by W. C. Stoll and J. M. Parker III 46 

Sheep Mountain mine, by E. Wm. Heinrich 47 

Shepherd Knob mine, by J. C. Olson . 48 

Stillwell mine, by J. C. Olson 50 

Tilley mine, by E. Wm. Heinrich 53 

Turkey Nest and Lyle Cut mines, by M. R. Klepper 54 


CONTENTS — Continued 




Figure 1. Index map showing location of the Franklin-Sylva 

district, N. C. L 2 

2. Structure Contours on top of pegmatite body, Big Ridge 
mine, Haywood County 30 

3. Map and sections of the Engle Cope mine, Jackson County- 36 
4. . Map of the Iotla-Bradley mine, Macon County 38 

5. Map and sections of the Rocky Face mine, Macon County ____ 47 

6. Map and section of the Tilley mine, Jackson County 54 


Plate 1. Map showing relation between Franklin-Sylva and 

Cashiers districts, N. C. 3 

2. Map of the Franklin-Sylva district, N. C, showing loca- 
tions of mines and prospects In pocket 

3. Map and sections of the Allman Cove mine, Macon County 21 

4. Map and sections of the Beasley No. 1 mine, Macon County__ 23 

5. Maps and sections of the Beasley No. 2 mine, Macon County.- 25 

6. Maps and sections of the Big Flint mine, Jackson County 27 

7. Map of the Big Ridge mine, Haywood County 29 

8. Sections of the Big Ridge mine, Haywood County 31 

9. Map and sections of the Bowers mine, Jackson County :___ 33 

10. Map and sections of the Cox mine, Jackson County 35 

11. Map and sections of the Kiser mine, Macon County 39 

12. Map and sections of the Lyle Knob mine, Macon County 41 

13. Map and sections of the Moody Mine, Macon County 43 

14. Map of the Poll Miller mine, Macon County 44 

15. Underground maps and sections of the Poll Miller mine, 
Macon County 45 

16. Map and sections of the Sheep Mountain mine, Jackson 
County 49 

17. Map and sections of the Shepherd Knob mine, Macon 
County 51 

18. Map and sections of the Stillwell mine, Jackson County 53 

19. Map and sections of the Turkey Nest mine, Macon County 55 


Raleigh, North Carolina 
March 9, 1946 

To His Excellency, Hon. R. Gregg Cherry, 
Governor of North Carolina. 


I have the honor to submit herewith, manuscript for publi- 
cation as Bulletin 49, "Mica Deposits of the Franklin-Sylva 
District, North Carolina," by J. C. Olson and others. 

From 1900 through 1940 North Carolina produced 60 per- 
cent of all the mica mined in the United States. The value of 
sheet mica produced in North Carolina in 1944 was 480 percent 
greater than that produced in 1941. 

The Franklin-Sylva district ranks second in total production 
among the mica mining areas of the Southeastern states and 
supplies approximately 20 percent of North Carolina's output. 
It is believed that the information contained in this report will 
be of value to the mining industry of the area covered. 

Respectfully submitted, 

R. Bruce Etheridge, 



This report entitled "Mica Deposits of the Franklin-Sylva 
District, North Carolina" has been prepared cooperatively by the 
U. S. Geological Survey and the N. C. Department of Conserva- 
tion and Development. It represents the work of twelve geologists, 
all of whom are properly credited either in the text or on the maps 
of the report. 

This report is a companion volume to Bulletin 43, "Economic 
Geology of the Spruce Pine District, North Carolina." These 
two reports, Bulletins 43 and 49, cover the major mica producing 
areas of North Carolina. While the Spruce Pine and Franklin- 
Sylva districts represent the most important of the State with 
respect to the volume and value of mica produced, there are 
several others of considerable importance. Most of these have 
been studied during the cooperative program and are being de- 
scribed in an over-all report being prepared for publication by 
the United States Geological Survey. 

Jasper L. Stuckey, 
State Geologist. 





By J. C. Olson 


The Franklin-Sylva district ranks second in total mica production among the mining areas of the 
Southeastern states. It is underlain almost wholly by metamorphic rocks that include mica, hornblende, 
garnet, and kyanite gneisses. The majority of the mica-bearing pegmatites cut across the foliation of the 
older rocks and were probably emplaced in fractures. Some of the bodies are more than 100 feet thick, 
but most are 5 to 15 feet thick. The plunges of pegmatite bodies are not consistent throughout the district. 

Mining is for mica almost exclusively, although feldspar has been the principal product of at least four 
mines. The heavy demand for mica during the war years has resulted in increased mining activity and 
made the time opportune for detailed study of the deposits. Large-scale maps have been prepared of many 
mica mines. 

The mica is commonly localized into certain parts of the pegmatite bodies, called "shoots" or "streaks," 
which are mined selectively. The position of the mica shoots varies among the different pegmatites. The 
mica blocks may be found clustered near quartz cores that make up a third or a fourth of the total thickness 
of some pegmatite bodies, near walls or inclusions, in sporadic "pockets", or disseminated throughout the 
pegmatite body. Granite and pegmatite occur together in five composite dikes. 

The quality of mica has been an increasingly important factor in all mica mining. Wartime demands 
have led to selective mining of the high-quality, flat, clear, easily-split sheet mica in sizes larger than 1 
square inch. Much of the Franklin-Sylva mica is clear and of rum (light-brown) or ruby color. Dark rum 
(brown) and green mica that is partly stained predominates along the southeast edge of the district and in 
the less-productive Cashiers district ten miles to the southeast. 

In the average sheet-mica mining operation, from 5 to 15 tons of rock are moved daily, yielding from 
a few to 500 pounds of block mica. Total mica in the rock mined probably ranges from 3 to 10 percent at 
most good mica mines, but if mine scrap and mica too small to be recovered are excluded, the remaining 
block mica probably averages only one to four percent of the rock mined. Feldspar mining has seldom been 
profitable in the district, owing to the high cost of transportation to the nearest market at Spruce Pine, but 
coarse potash feldspar occurs in some of the pegmatites. « 

It is estimated that the Franklin-Sylva district has supplied nearly 20 percent of North Carolina's out- 
put of mica during the period 1920 to 1940. About half of this was from the Big Ridge mine. The average 
annual output of the district for the years 1920-40 is estimated as nearly 126,000 pounds of sheet and 
punch mica. There is no geologic reason why this rate of production should not remain approximately the 
same under similar economic conditions. The rate of production attained during the war years 1942-44 is 
the best index of the district's potentialities under more intensive development. 


The importance of mica to the nation during the war has resulted in great expansion of mica mining in 
the Franklin-Sylva district as well as other domestic mica-producing areas. Many old mica mines have been 
reopened and new prospects developed. The intensive mining activity has exposed many pegmatites and 
made the time opportune for detailed geologic study of the deposits. Detailed mapping of mines and geo- 
logic study of the mica occurrences have been very useful both in the evaluation of specific deposits and as 
a guide in their development. The geologic work on which this report is based was designed primarily for 
immediate use as a guide to mining operations, but the data obtained on the geology and extent of mine 
workings should be of practical value in the future as well. 

2 Mica Deposits of the Franklin- 

To facilitate the production of domestic mica, the Colonial Mica Corporation was established in 1942 as 
an agent of Metals Reserve Company. During the period of great demand and unusually high prices, the 
Colonial Mica Corporation became the sole purchasing agent for high-quality sheet and punch mica in this 
country. The Corporation has aided miners by supplying them equipment at nominal rentals, by advancing 
funds to be used in opening promising mines or prospects, and by providing men experienced in the mica 
industry to advise operators on the mining and preparation of mica. 


The Franklin-Sylva pegmatite district, in southwestern North Carolina, includes parts of Macon, Jack- 
son, Haywood, and Transylvania counties. (See fig. 1.) The southwest boundary of the district is arbi- 
trarily taken as the line between Macon and Clay counties, but scattered deposits have been mined in Clay 

Fig. 1. — Index Map Showing Location of the Franklin-Sylva 

District, N. C. 

County and northeast Georgia. The Franklin-Sylva district is a northeast trending belt 14 miles wide and 
45 miles long, in which hundreds of pegmatites have been mined or prospected for mica. This district 
ranks second in total mica output among the mining areas of the Southern Appalachian region ; feldspar, 
kaolin, corundum, garnet, dunite, copper, and vermiculite have also been mined. 

The Cashiers district, another area in which many mica-bearing pegmatites occur, lies southeast of the 
Franklin-Sylva district. In a few places the two districts almost join, as shown in plate 1, but elsewhere 
they are separated by a relatively barren area in which very few mica-bearing pegmatites occur. This re- 
port deals primarily with the Franklin-Sylva district, but also contains a discussion of its geologic relations 
to the less productive Cashiers district. The locations of mines in the Franklin-Sylva district are shown in 
plate 2. 

The Franklin-Sylva district is in the Appalachian Mountain region, among transverse ridges that lie 
between the Blue Ridge on the southeast and the Smoky Mountains on the northwest. Altitudes range from 
1,950 feet on the Tuckasegee River to 6,540 feet on Richland Balsam. Much of the district is mountainous, 
but basin-like areas one to four miles wide along the principal rivers are characterized by gently rolling 
topography. The rocks are commonly weathered, in places to depths of more than 100 feet. Hard out- 
crops are most abundant on the steeper slopes. The principal streams, the Pigeon, French Broad, Tuckase- 

Sylva District, North Carolina 




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i— i 





>— i 






4 Mica Deposits of the Franklin- 

gee, Little Tennessee, and Nantahala Rivers, are upper tributaries of the Tennessee River, which flows west- 
ward into the Ohio River near its junction with the Mississippi. 

The district is served by the Murphy Branch of the Southern Railway, which passes through Canton, 
Waynesville, and Sylva. The southwest part of the district is also served by the Tallulah Falls Railway, 
connecting Franklin with the Southern Railway at Cornelia, Georgia. Federal and State highways and many 
county roads make all parts of the district readily accessible. 

The Colonial Mica Corporation has maintained an office in Franklin and a mica-trimming and buying 
shop in Sylva to serve the Franklin-Sylva district. Other plants utilizing pegmatite minerals at the present 
time (October 1944), are four scrap-mica plants near Franklin and many mica-trimming shops for prepa- 
ration of sheet mica mined in the district. 


This report is based upon field work done by the Geological Survey, U. S. Department of the Interior, 
in cooperation with the North Carolina Department of Conservation and Development. The work has been 
carried on intermittently since June 15, 1942, and is still continuing (October 1944). The investigations 
during 1942 consisted of reconnaissance examination of 254 mica mines and prospects and the detailed map- 
ping of two of the largest mines. In 1943 and 1944 detailed geologic maps were made of 64 individual de- 
posits, and many others were examined. The mine mapping was done on scales ranging from 20 to 50 feet 
to the inch. Control for surface mapping was obtained by plane-table and alidade, whereas underground 
surveying was done by compass and tape methods. The following geologists have participated in this work : 


J. C. Olson June 15 to November 30, 1942. 

February 19-24 and March 5-10, 1943. 

May 23 to August 6, 1944. 

J. J. Page June 20 to September 7, 1942. 

W. C. Stoll February 8 to June 1, 1943. 

J. J. Norton February 8 to 20, 1943. 

J. M. Parker, III February 19 to July 4, 1943. 

V. C. Fryklund, Jr June 24 to July 4, 1943. 

D. M. Larrabee December 6, 1943 to February 10, 1944. 

M. R. Klepper December 6, 1943 to May 12, 1944. 

W. B. Allen December 13 to 31, 1943. 

E. Wm. Heinrich January 4, 1944, to ? 

L. C. Pray January 1944 to May 19, 1944. 

R. W. Lemke July 27, 1944, to ? 

The investigations in 1942 were under the general supervision of G. R. Mansfield; during 1943 and 
most of 1944 they were under the general direction of H. M. Bannerman and from the latter part of 1944 
to the present they have been directed by E. N. Cameron. R. H. Jahns, who has been in charge of pegmatite 
studies in the Southeast since May, 1944, made helpful criticism of the manuscript and illustrations. E. Wm. 
Heinrich prepared many of the illustrations as well as mine descriptions. The writer is indebted to Dr. J. L. 
Stuckey, State Geologist of North Carolina, for his interest and wholehearted cooperation in the work. 

Colonial Mica Corporation, agent for Metals Reserve Company, has given full cooperation as well as 
much information of value to the present study. W. E. Grindstaff of the Asheville Mica Company kindly 
furnished records of mica sales over a 20-year yeriod. Many miners and other residents of the district have 
given information regarding mining history and the location of mines. 


The geology of much of the Franklin-Sylva district has been described by Keith 1 , and many of the mica 
deposits have been described by Sterrett 2 . 

'Keith, Arthur, U. S. Geol. Survey, Geol. Atlas, Pisgah (No. 147) and Nantahala (No. 143) folios. Cowee quadrangle (un- 
" Sterrett, D. B., Mica deposits of the United States: U. S. Geol. Survey Bull. 740, 1923. 

Sylva District, North Carolina 5 



The district is underlain almost wholly by metamorphic rocks, mapped by Keith 3 as the Carolina (domi- 
nantly micaceous) and Roan (dominantly hornblendic) gneisses. Several varieties of mica gneiss are inter- 
layered in various proportions. They range in composition from schist that is rich in muscovite, with a 
little quartz, feldspar, and biotite, to the more abundant quartzose mica gneiss in which the mica flakes are 
sparsely distributed. Garnet and kyanite are prominent in some of the gneisses. A few fine-grained grani- 
toid layers occur among the other rock types. 

Feldspathic gneisses are commonly interlayered with the other rocks. In places the schistose rocks 
contain much introduced quartz and feldspar, as pods or lenses from a fraction of an inch to several inches 
in thickness, especially near larger pegmatite bodies. Much of the gneiss and schist in the vicinity of 
granite bodies in the Cashiers district appears to have been permeated by pegmatitic and granitic solutions. 
Small pods, lenses, and stringers of pegmatite along the foliation planes of metamorphic rocks are much 
more common in the Cashiers district and the southeast part of the Franklin-Sylva district than they are 
in the main belt of Franklin-Sylva mica deposits. 

Hornblende gneiss and schist occur both as layers from a few inches to 100 feet thick in the micaceous 
rocks and as larger units mapped as Roan gneiss by Keith. The hornblende schist consists mostly of black 
hornblende needles, about one-tenth to one-half an inch in length, with quartz, feldspar, and a little biotite. 
The hornblende gneiss is a banded rock composed of alternating dark (hornblendic) and light (quartz-feld- 
spar) layers. 

The micaceous schist and gneiss are largely of sedimentary origin. Some of the hornblendic rocks may 
be sills, but their interlayering with diverse rock types and the absence of cross-cutting relations suggest 
that they probably are largely of volcanic or sedimentary origin. 


The best outcrops are found on the steep slopes, and are composed predominantly of mica-garnet gneiss 
and kyanite gneiss. Most of the rock in the topographic basins near the rivers is weathered deeply, yielding 
light-red to reddish-brown and brown to brownish-yellow soils. In general the hornblendic rocks yield red 
clay soils, although some are yellowish brown. The mica and garnet gneisses yield yellow, brown, and gray 
soils. Red soils are more plentiful in the valleys and plateaus, presumably because the weathering is more 
advanced and the iron-bearing minerals therefore more oxidized. 



Coarse-grained granite, in part pegmatitic, underlies areas as much as 18 miles long and 5 miles wide 
in the Cashiers district, and extends south westward into Georgia and South Carolina. (See pi. 1.) This 
rock was called the Whiteside granite by Keith 4 . It is light colored and is composed of quartz, orthoclase 
and plagioclase feldspars, and a little muscovite and biotite. Patches and streaks of coarser pegmatite of 
similar composition occur within the granite. The principal granitic intrusions are thick sill-like bodies 
that appear to have bulged the overlying metamorphic rocks upward. Many thin sills of granite occur, in 
the adjacent mica gneiss, and slab-like inclusions of gneiss are common in the granite. The gneisses have 
been permeated with quartz and feldspar over large areas near the granite. The granite resembles that at 
Spruce Pine 5 , in its texture and structural relation to the metamorphic rocks. 

OTHER granitic bodies 

Fine- to medium-grained biotite granite occurs in large and small areas several miles northwest of the 
Franklin-Sylva mica belt. It is unlike the Whiteside granite, and has been correlated with the Cranberry 

3 Keith, Arthur, op. cit. 

1 Keith, Arthur, Pisgah folio: U. S. Geol. Survey Geologic Atlas, No. 147, 1907. 

6 Hunter, C. E., Residual alaskite kaolin deposits of North Carolina: Amer. Ceramic Soc. Bull., vol. 19, no. 3, pp. 98-103, 
March 1940. 

Olson, J. C, Economic geology of the Spruce Pine pegmatite district, North Carolina: North Carolina Dept. Cons, and 
Devel. Bull. 43, 1944. 

6 Mica Deposits of the Franklin- 

granite by Keith 6 . Its largest area of outcrop is north and west of Canton, but smaller bodies occur in the 
Nantahala Mountains and north and west of Franklin. 

Granitic dikes are sparsely distributed in the district as a whole, but are most plentiful in the north- 
east and central part. Most of them are between three inches and six feet thick, and are composed of fine- 
grained feldspar and quartz, fine muscovite and biotite flakes that are commonly parallel to one another, 
and scattered small garnets. Porphyritic varieties have medium- to coarse-grained feldspar, quartz, or bio- 
tite, in a finer-grained matrix. Fine-grained, slightly foliated granite dikes, eight inches to five feet thick, 
are best exposed at the Sally Reed, Bee Tree No. 1, Rock, Diller Bryson, and Island Ford mines. Most of 
them cut the pegmatite bodies and are doubtless younger, although the difference in age may not be great. 
Aplite dikes are cut by pegmatite at the Iotla-Bowers mine. They are two feet thick on the average, uni- 
form in grain size, and composed of an intimate mixture of quartz and kaolinized feldspar. 

Granite and pegmatite occur together and are genetically related in the composite dikes at the Tilley, 
Roarenhole, Moss, Borrows Cut, and Big Ridge pegmatites. The granite and the pegmatite in these unusual 
deposits were formed at essentially the same time. The granite, described on p. 10, is fine- to medium- 
grained and is distinctly different from the coarse-grained Whiteside granite. 


Small bodies of ultrabasic rocks occur in the district. They are generally elliptical in plan, having a 
maximum width of as much as 0.4 mile, and a maximum length of more than 2 miles 7 . They are most 
extensive in the Webster-Addie-Balsam area of Jackson County. As Hunter points out, the individual 
bodies in the Webster-Addie area are arranged along the circumference of a circle, forming a discontinuous 
ring-dike. Numerous isolated dunite bodies occur in other parts of the district. Dunite, consisting almost 
entirely of olivine, and an impure soapstone containing amphiboles are the most common varieties. The 
dark, rocky ground where they occur supports little vegetation. These rocks were observed by Keith 8 to cut 
across the Roan gneiss. 



The planes of schistosity have been folded on a large and small scale. The schistosity strikes rather 
uniformly northeast over much of the district, but local deflections to a northwest strike are not uncommon. 
Almost all the foliation in the Franklin-Sylva district dips at an angle greater than 45 degrees and much is 
approximately vertical. In the Cashiers district the dips are less steep on the average, many of them less 
than 45 degrees. The decrease of dip southeastward is similar to that in the Spruce Pine district 100 miles 


Fracturing of the metamorphic rocks has an important bearing on the distribution of commercial mica 
because fractures formed prior to pegmatite introduction guided the incoming solutions and, in pegmatite 
already solidified, rock movements crush or "rule" the mica. Faults and joints are numerous in the Franklin- 
Sylva district, but the faults observed are probably not of very great displacement. Some of the fractures 
have been filled with quartz or pegmatite. 

The general character of the fracturing may be seen in a road cut about 200 feet long on Savannah 
Creek. There the strike of the foliation of the gneiss is nearly uniform in the cut, but the dip changes 
abruptly within short distances because of close folding. Four parallel pegmatite bodies one to two feet 
thick cut the gneiss. They dip steeply, have sharp walls, and presumably fill fractures. A gently-dipping 
normal fault, along which drag is evident, cuts the gneiss. This fault has been filled with quartz, but other 
small faults exposed have no filling. In general this example is thought to typify the structure of the 
district. Steeply-dipping, parallel pegmatite bodies, emplaced in fractures, cut the country rocks. Later 

• Keith, Arthur, op. cit. 

7 Hunter, C. E., Forsterite olivine deposits of North Carolina and Georgia: North Carolina Dept. Cons, and Devel. Bull. 41, 

9 Keith, Arthur, op. cit., p. 3. 

Sylva District, North Carolina 7 

faults cut wall rocks and pegmatite. These post-pegmatite faults are numerous in the Savannah section of 
Jackson County, but they occur throughout the district. They have effected much ruling and bending of the 
mica books. 

Many contact relations indicate that pre-pegmatite faults were channels for incoming solutions. Sharp 
changes in strike of foliation a few inches to three feet from the pegmatite body may be the result of drag 
along a fault prior to the introduction of pegmatite. Evidence of such drag was observed at the R. T. 
Bryson, Poll Miller, Winecoff, Dills, Lin Cove, Wilkes, and other mines. At the Jack Knob mine, for example, 
the foliation of the biotite gneiss at the contact is very nearly parallel with the walls of the pegmatite body, 
but it changes two feet from the contact from a northwest strike to nearly due east, through an angle greater 
than 90 degrees. 

Fractures in the metamorphic rocks undoubtedly controlled the disposition of many of the pegmatites. 
This control is indicated by the parallelism of tabular discordant pegmatite bodies, for example those in the 
Panther Knob area of Jackson County and those in a belt extending three miles northwest from the town of 
Franklin. Abrupt bends in cross-cutting pegmatite bodies, and offshoots or apophyses having diverse atti- 
tudes, provide additional evidence of the existence of a pre-pegmatite fracture pattern. 

Contacts between pegmatite and wall rock are comparatively sharp in the nearly tabular pegmatite 
bodies that appear to have formed in fractures. Not all the pegmatite bodies are tabular or so sharply 
defined, however, for some have very irregular walls. Notable examples of irregular-walled pegmatite 
bodies are the Burr Knob, Iotla-Bradley, Gurney Clay, Shepherd Knob, and Dillard mines. 

The effect of pre-pegmatite fracturing of the rocks is more pronounced in the Franklin-Sylva district 
than it is to the southeast in the Cashiers district. The invasion of the granitic magma near Cashiers was 
accompanied by profound "soaking" of the metamorphic rocks, and schistosity was most important as a 
guide to incoming pegmatitic and granitic solutions. 



The pegmatite bodies range from lenses a fraction of an inch thick to great masses such as the Big 
Flint, Iotla-Bradley, Shepherd Knob (each 100 feet or more thick), Lin McCall (50 feet), Roda (about 150 
feet), Gradin (65 feet), and Gurney Clay (50-200 feet). Thicknesses vary, but some pegmatite dikes that 
appear to have formed in fractures are nearly uniform in thickness for 100 feet or more along the strike. 
Many pegmatite bodies are lenticular, and thin rapidly along the strike. For example, the thickness of the 
"Little Vein" at the Welch mine diminishes from 4 feet to 5 inches within a strike distance of 20 feet. The 
quartz core and associated mica are present where the pegmatite body is 4 feet thick, but not where it is 
only 5 inches thick. 

The pegmatite bodies have a variety of shapes. Some are tabular or sheet-like (Frady) ; some are 
elongate lenses (Iotla-Bowers) ; some are very irregular (Shepherd Knob, Dillard). Some vein-like quart- 
zose bodies are thin and have irregular gradational contacts (Rock, Cedarcliff, and Bee Tree No. 1) ; others 
are merely small lenses, some without visible connection, disposed along a plane or in imbricate arrangement 
in the gneiss or schist. At the Island Ford mine, for example, lenses one to three feet thick were mined 
along a thin, conformable layer of gneiss that contained many pods and stringers of pegmatite material. 
Books of mica have been found here in the wall rocks of gneiss. 


Most of the pegmatite bodies dip steeply, and the majority cut across the foliation of their wall rocks. 
Some strike parallel to the foliation, but transect it in dip ; this type is particularly common in an area of 
several square miles northwest of Franklin. "Rolls", or abrupt changes in dip, are common. 

The pegmatite and associated granite body at the Big Ridge mine (see description, pp. 28-32) are arch- 
shaped, as is the pegmatite body at the Cox mine (pp. 32-34) . A somewhat similar bend occurs in the Shep- 
herd Knob pegmatite (described on pp. 48-50). In all these deposits, at least one of the limbs of the arch 
crosscuts the wall-rock foliation. The arched shape is apparently due to the arrangement of intersecting 

8 Mica Deposits of the Franklin- 

fractures that guided the solutions, and not to subsequent folding of both pegmatite and wall rock or to the 
introduction of solutions conformably along the crest of an anticlinal fold in the gneiss. 

The plunges of pegmatite bodies are not consistent throughout the district. Many of the tabular bodies 
have been mined directly down the dip, whereas in the Spruce Pine district to the northeast the predominant 
plunge of pegmatite bodies is toward the south or southwest at angles of 20 to 40 degrees. Plunges other 
than directly down dip have been established for at least a dozen Franklin-Sylva pegmatite bodies, or parts 
of the bodies, including the following: Baird (one of several pegmatites on property), plunges 30° SE. to 
horizontal; Beasley No. 2, 35° SE.; Bowers, 45° NW.; Buoy No. 1, 20° NW. to 60° NW.; Buoy No. 2, 25° 
NW.; Cox, 10° S68°W.; Lyle Knob, 25° W.; May, 25° N45°W.; Moody, 60° S55°W.; Poll Miller, 24° NE. to 
40°NE.; Raby, 47° S82°E.; Shepherd Knob, 15°N. to 20°N. The diversity of direction suggests that such 
plunging structures are related to local rather than regional structural elements. 


The metamorphic wall rocks or inclusions may be altered by pegmatitic solutions both through the 
coarsening of mineral grains in the gneiss or schist, and through the addition of pegmatite minerals. Small 
lenses of quartz or feldspar are common in wall rocks, especially in the more schistose varieties. Pyrite 
and pyrrhotite occur in wall rocks, particularly adjacent to certain quartzose pegmatites. Examples of the 
coarsening of wall-rock minerals are numerous. At the Shepherd Knob mine, for example, the rocks near 
the pegmatite are markedly different from the more normal country rock exposed in adits 200 to 300 feet 
away. There are several types of wall-rock alteration at the Shepherd Knob: (1) mica books as much as 
1.5 inches in diameter are present in the wall rocks and inclusions, generally with their cleavages perpen- 
dicular to the foliation and enclosing many small garnets; (2) the wall rock has been permeated with peg- 
matitic feldspar and quartz; and (3) the mica gneiss has become enriched in mica and thereby changed to 
mica schist. The first two types of alteration yield a rock that is gradational between true pegmatite and 
wall rock. 


The pegmatities of the Franklin-Sylva and Cashiers districts contain microcline and plagioclase feld- 
spars, quartz, muscovite, biotite, garnet, allanite, apatite, magnetite, tourmaline, ankerite, beryl, samarskite, 
hedenbergite, and such sulfide minerals as pyrrhotite, pyrite, and, chalcopyrite. 

Most of the quartz in the Franklin-Sylva district is white or sugary. A little is gray or smoky, but 
gray quartz is more abundant in the Cashiers pegmatite belt to the southeast. Veins of white quartz contain- 
ing a little ilmenite and iron oxide are common in all the country rocks. They range from a fraction of an 
inch to about four feet in thickness. 

Potash feldspar (microcline) is the dominant feldspar in many of the pegmatites, but plagioclase pre- 
dominates in most mica-bearing streaks. It is often difficult to distinguish feldspars because they are almost 
completely altered to kaolin in the surficial portions of many pegmatites. Graphic intergrowths of quartz 
and feldspar (graphic granite) are rare. 

Biotite is an abundant pegmatite mineral, and much of it is intergrown with muscovite. In some peg- 
matites it occurs as long strips — as much as five feet long at the Putman mine. Biotite probably constitutes 
at least a third of the mica at the Big Ridge mine, and at the J. Radeker mine it appears to be l 1 /^ to 2 times 
as abundant as muscovite. It is exceptionally plentiful at the Ray Cove mine, in blocks as large as 6 x 8 x % 
inches. Perhaps its abundance here is due partly to interaction between the pegmatite and hornblende- 
garnet gneiss, which forms the wall rock at this mine but at very few others. The pegmatite at the Sheep 
Mountain mine, whose wall rock is quartz-biotite gneiss, is exceptional in having a large proportion of both 
biotite and muscovite. (See description, pp. 47-48.) Some of the biotite strips occur near the margins of. 
massive quartz bodies — for example in the Moody mine (p. 42) and the Big Flint (pp. 26-28). 

Garnet is sparsely distributed in the pegmatites, but it occurs in 2-inch crystals at the Blanton prospect. 
Apatite and allanite occur in a few pegmatites. Black tourmaline is found at the Painter mine, and at the 
Slagle mine at Rainbow Springs. Black and pink tourmaline, samarskite, and beryl have been reported by 
J. H. Pratt 9 from the Grimshawe mine in the Cashiers district. There is little or no beryl in the Franklin- 
Sylva district, but some gem material has been mined in the Cashiers district. 

' Sterrett, D. B., op. cit., p. 216. 

Sylva District, North Carolina 9 

Sulfide minerals are widely distributed, and commonly occur in quartzose pegmatites or in massive 
quartz bodies in larger feldspathic pegmatites. Pyrrhotite and pyrite are plentiful in the quartzose peg- 
matites at the Bee Tree No. 1, Rock, Cedarcliff, and Shiny mines. Chalcopyrite and bornite occur with the 
more common pyrrhotite and pyrite at the "C" mine, and masses of pyrrhotite with chalcopyrite, weighing 
as much as a half-pound, occur at the Thorn Mountain mine. Veinlets of sulfide minerals at the Tilley mine 
cut all the other minerals. The sulfide minerals appear to be among the last to form in the sequence of peg- 
matite minerals. 


The economic value of a pegmatite body depends to a great extent upon the degree to which the minerals, 
particularly mica, are localized or concentrated into "shoots" or "streaks". Pegmatites in the Franklin- 
Sylva district in which the minerals are distributed more or less uniformly seldom can be mined profitably 
for sheet mica. Mineral proportions vary along the strike or down the dip of a pegmatite body. The mining 
is usually done in parts of the pegmatite bodies where the valuable minerals are most conspicuously localized. 


Massive quartz forms the central part, or core, of many pegmatite bodies, commonly comprising a fourth 
to a half of the total thickness of a dike. The quartz mass at the Big Flint mine is as much as 65 feet thick 
(see pi. 6) ; that at the Shepherd Knob mine is at least 20 feet thick (pi. 17). The quartz bodies have the 
form of irregular lenses, somewhat elongate in the direction of plunge of the pegmatite body. In shape they 
range from attenuated, almost tabular lenses (Poll Miller mine, pis. 14 and 15; Turkey Nest and Lyle Cut 
mines, pi. 19) to lenses with thickness nearly equal to strike length (Big Flint mine, pi. 6; Roda mine). 
Many are discontinuous and are distributed unevenly along the strike or plunge of the pegmatite body. 

The thickest part of many of the quartz cores coincides with the thickest part of the enclosing peg- 
matite bodies and, in places, with abrupt bends in strike or dip of the pegmatites. The thick quartz mass at 
the Moody mine (pi. 13), for example, occurs in a segment of the pegmatite that trends N.60°E., whereas 
both east and west of this segment the strike is slightly north of west and the pegmatite is not so conspicu- 
ously zoned. Likewise the parts of the Moody pegmatite richest in mica, where the quartz is thickest, may 
coincide with a slight decrease in the dip of the pegmatite body. A quartz core in the thickest part of Iotla- 
Bowers pegmatite coincides with an abrupt change in strike of the footwall from N.60°W. to N.8°W. In 
general this dike dips steeply southwest and is practically homogeneous except for small scattered quartz 
pods and a slightly higher mica content along the footwall than in other parts. The deposit has been mined 
most intensively in a segment with a strike length of about 50 feet, in which the quartz core occurs. 

The typical quartz core is thickest near the central part of its strike length. In places (Raby, Welch 
mines) the quartz cores end very bluntly in plunging noses. In other pegmatites the quartz cores thin 
gradually until so small that they become indistinguishable among the other grains in the pegmatite. Beyond 
its vanishing point the quartz core may be succeeded by or grade into another central zone that differs from 
the wall zones; for example, the quartz mass in the middle of the Beasley No. 2 pegmatite (pi. 5) disappears 
along the strike and is supplanted by a plagioclase-mica pegmatite that differs from the wall zones in contain- 
ing much muscovite and biotite. At the Stillwell mine (pi. 18) the quartz core exposed at the base of the 
123-foot New shaft grades southward into quartz-muscovite pegmatite ("burr rock"), and northward into 
quartz-feldspar pegmatite. At the Poll Miller mine (pis. 14 and 15, description on p. 46) the quartz core is 
supplanted to the southwest by a thick central rib of coarse blocky microcline, which in turn grades into 
medium-grained feldspar-quartz pegmatite. Block muscovite is abundant in the wall zones at the Poll Miller 
both where the central part of the dike is quartz and where it is coarse microcline. 


Pegmatitic quartz containing many small (Vi to 1 inch), sub-parallel mica flakes is known locally as 
"burr rock". At the Shepherd Knob mine the "burr rock" appears to be a marginal phase of the large quartz 
core. At the Allman Cove mine (pi. 3), however, "burr rock" is more common than massive quartz, which is 
confined to small masses two or three feet thick near the west end of the mine. The bodies of "burr rock" 
range from an inch to a foot or more in thickness and are discontinuous. "Burr" streaks lie parallel to and 
within a few feet of each wall of the Allman Cove pegmatite, and another, near the middle, also follows the 

10 Mica Deposits of the Franklin- 

east trend of this pegmatite ; others have a northeasterly trend. Sheet mica occurs either in the "burr rock" 
or in the adjacent plagioclase. Much of the mica produced from the Miller mine was derived from "burr 


Fine-grained border zones generally less than a foot thick are present along the walls of many pegmatite 
bodies. The border zones are mostly plagioclase and quartz, but also contain mica flakes y± to 1 inch in di- 
ameter and small garnets in some places. The cleavage planes of the mica flakes tend to be perpendicular to 
the contacts. The grain size increases inward from the walls. 


The parts of the pegmatite bodies other than the border zones and the massive quartz cores will be con- 
sidered herein as "feldspathic pegmatite", inasmuch as feldspar is the predominant mineral except in rare 
varieties of quartzose pegmatite. Various kinds of feldspathic pegmatite may be distinguished according to 
the proportions of microcline, plagioclase, quartz, and other minerals. Numerous examples of feldspathic 
pegmatite are shown on the mine maps accompanying this report. It is possible in most pegmatite bodies to 
distinguish more than one type of feldspathic pegmatite, although this distinction is difficult when the feld- 
spars are weathered. A common distinction is that made between plagioclase-quartz pegmatite and micro- 
cline-quartz pegmatite. The microcline-rich parts of the pegmatite bodies are generally in the interiors, 
whereas the plagioclase-rich parts tend to occur along the margins. Commercial muscovite is most abundant 
in the plagioclase-quartz type. 


Granite that forms a component part of the composite dikes at the Tilley, Moss, Borrows Cut, Roaren- 
hole, and Big Ridge mines differs from the large granite bodies and granitic dikes described on previous pages. 
The granite at each of these five mines is a uniformly fine-grained mixture of oligoclase, quartz, and biotite. 
Although the rock contains very little potash feldspar, it will be referred to in this report by the miners' 
term "granite". 

The composite dike exposed at the Moss (Adams) mine consists of a central granite body three feet 
thick, along each margin of which occurs a six-inch to two-foot thickness of fine-grained pegmatite. This 
dike is exposed discontinuously from the south end of the mine, where it is V/2 feet thick, to a point a third 
of a mile to the north on the Tuckasegee River. Most of the mining was done, however, within a strike dis- 
tance of 800 feet ; Sterrett 10 has described the pegmatite in the main workings. The pegmatitic zones consist 
in some places almost entirely of muscovite, in others of feldspar and some quartz. The contact between the 
pegmatite and the granite, according to Sterrett, is irregular and not sharply defined. Many of the mica 
crystals, especially near the walls, have cleavage planes normal to the contacts. 

The granite and pegmatite at the Big Ridge mine are described on pp. 28-30. Here the mineralogic rela- 
tions indicate that much of the pegmatite crystallized later than much of the granite, although the difference 
in age is not great. In some places the granite was probably the earliest material intruded along the irregular 
fractures, as it forms part of the wall rock of the pegmatite ; in one place, at least, the granite was the last to 
form, for a dike 8 inches thick cuts sharply across both pegmatite and earlier granite. 

At the Borrows Cut, a dike 5 feet thick has a core 21/2 feet thick of quartzose fine-grained granite in 
which biotite flakes and streaks have parallel orientation. The pegmatitic border zones of this composite 
body are crowded with small mica books as much as 5 inches in diameter. The granite and pegmatite at the 
Tilley mine are described on p. 54. 


Muscovite occurs sporadically in most pegmatites, but where mineable, the blocks are large and clustered 
into certain rich "streaks" or "shoots". Table I summarizes the prevailing modes of occurence of mica in the 170 
mines in the Franklin-Sylva district in which the localization of the mica could be either observed or inferred. 

10 Sterrett, D. B., op. cit., p. 202. 

Sylva District, North Carolina 11 

They include for the most part the best-exposed pegmatites and those that have the most clearly defined mica 
concentrations. Many other pegmatites are difficult to classify because of absence of mica or of pegmatite 
exposures. Difficulties arise in such a classification either because of the presence of more than one type of 
mica concentration in a single deposit, because the mica is not definitely concentrated, or because incomplete 
exposures in many places do not give a full picture of the pegmatite body. Observations are sufficiently 
numerous, however, to make the table of value in demonstrating the proportions of the various mica oc- 


Mica blocks or clusters of blocks disseminated through a pegmatite body rather than in a well-defined 
streak or zone are not likely to be mined profitably for sheet mica. Some weathered bodies of this type, how- 
ever, have been important sources of scrap mica. Scrap mica is abundant in the felpspathic pegmatite at the 
Iotla-Bradley mine (fig. 4), averaging about 10 percent of the rock and forming as much as 50 percent in 
places near quartz bodies. A little mica occurs in the quartz. This and similar pegmatites are classed with 
the disseminated deposits because of the presence of mica in such a large part of the pegmatite body, even 
though numerous scattered concentrations occur locally. 

Scattered clusters of mica blocks occur sporadically in some small, irregular pegmatite bodies. Most 
mica at the Bettys Creek mine, for example, is found in thicker parts (as much as 6 feet thick) of the bodies, 
and bears no apparent relation to the small quartz bodies or to the walls. Other mica pegmatites in which 
the mica is disseminated or sporadic are the Putman, Gibson, Burr Knob, Oscar Queen, and Gurney Clay 

table i 

Summary of Mica Localization in Pegmatites of the Franklin-Sylva District 

Number of Approximate 

Type of mica occurrence examples percent 

Disseminated and sporadic distribution 9 5 

Quartz core present: 

Mica near quartz core 68 40 

Mica near walls 24 14 

Mica near both quartz core and walls 29 17 

Quartz core absent or inconspicuous: 

Mica near one wall 15 9 

Mica near both walls 15 9 

Mica near inclusions and walls 5 3 

Mica possibly related to granite bodies within 

or in contact with pegmatite 5 3 

Total 170 100 


The relation of mica shoots to quartz masses makes the margins of quartz bodies favorable for prospect- 
ing. As a general rule, rich mica shoots related to quartz cores tend to occur alongside the thickest parts of 
quartz masses. A thick quartz core, however, does not necessarily indicate a concentration of mica, for 
quartz bodies are much more numerous than rich mica streaks. 

The disposition of the mica blocks with respect to the quartz bodies varies among the different deposits. 
In some the mica occurs throughout a thin zone between quartz and wall, but generally it is localized near 
either quartz or walls. In the majority of the quartz-core pegmatites, the mica blocks are clustered near the 
quartz. At the Raby mine, some mica crystals cross the contact between quartz and adjacent feldspathic 
pegmatite. Crystal faces are developed on the parts of the books projecting into the quartz, whereas the 
margins of the same books in feldspathic pegmatite (now kaolin) are ragged and irregular. 

The mica blocks may be found more or less continuously along the margins of the quartz, but more com- 
monly they are clustered in "shoots" or "pockets" separated by leaner feldspathic material. The long dimen- 
sions of some "shoots" can be correlated with the plunge of structural features such as flexures ("rolls") in 
the walls of the pegmatite body, which generally parallel the plunge of the pegmatite body as a whole. Mines 

12 Mica Deposits of the Franklin- 

at which the mica blocks adhere closely to quartz cores are the Beasley No. 1, Lyle Cut, "A", Iotla-Bowers, 
Raby, Moody, Shepherd Knob, and Locust Tree. The size of the mica blocks generally diminishes away from 
the quartz mass. 

Different from the above-described pegmatites are those in which the coarser mica blocks lie near the 
walls rather than near the central quartz body. Feldspathic zones with very little mica border the central 
quartz mass, and are composed of either coarse plagioclase or plagioclase with blocky microcline. Angular 
feldspar grains project into the massive quartz. At the Beasley No. 2 mine the coarsest mica blocks are 
separated from the hanging wall of the dike by a 6- to 12-inch border zone of medium-grained plagioclase, 
quartz, and mica- (see discussion, p. 24) ; coarse oligoclase adjoins the massive quartz. Other examples of 
quartz-core pegmatites having mica near the walls are the May, Buoy No. 2, Painter, Bowers, Deets, Locust 
Ridge, and Gregory. The cleavage of the muscovite in some of these pegmatites shows a striking tendency 
to lie perpendicular to the walls, for example the Frady (p. 37) and Stillwell (p. 52) mines. 

The occurrence of muscovite-rich zones along both quartz and walls is not uncommon. Examples are 
the Roda, W. G. Dillard, Doc Nichols, and Chalk Hill mines. At the Lin McCall mine, stained green wedge 
mica occurs near quartz masses, whereas clear and stained dark-rum mica occurs near the footwall. Mus- 
covite has been mined near the quartz core in one pegmatite at the Baird mine; in another on the same 
property it occurs near the walls. 

Muscovite generally occurs in plagioclase-rich pegmatite, in the Franklin-Sylva district as in other mica- 
producing pegmatite districts. 11 At the Farlow Gap mine, for example, coarse muscovite occurs near the walls 
in plagioclase pegmatite rather than in the quartz-microcline core. The central part of the Lyle Knob peg- 
matite body (pi. 12) is massive quartz, in places containing abundant microcline. Mica is concentrated near 
the walls of the pegmatite body where the percentage of plagioclase in the rock is higher. 

Inasmuch as microcline tends to occur in the central parts of the zoned pegmatites of the Franklin-Sylva 
district rather than the margins, muscovite in a microcline-rich pegmatite would be most likely to occur nearer 
the walls. If microcline is scarce or absent, of course, mica may be found in plagioclase-rich zones near 
either walls or massive quartz cores. 

Differences in mica content on the two sides of a quartz core are common. Mica at the Judge Ferguson 
mine was obtained mostly on the south side of a quartz mass four feet thick in a vertical pegmatite body 12 
feet thick. Where the distribution is uneven, mica is generally more abundant on the upper side of the 
quartz. Differences in quality and color on the two sides of the quartz apparently exist also. For example, 
in the Long Branch and Gregory mines ruby mica occurs on the upper, whereas greenish-white specked 
mica occurs on the lower, side of the quartz bodies; in the Spence ruby mica on the upper side, and biotite 
near the footwall ; in the Double Gap clear, rum mica on the upper side, and stained greenish-rum on the lower ; 
and, in the Ramsey Buchanan clear mica on the upper side, and slightly stained on the lower. Two types of 
mica occur at a number of other mines in the Savannah section of Jackson County, including the Wilkes, 
Kolb, and Collins, but the positions of the two types within these pegmatites is not known. In all the above 
occurrences of two colors of muscovite, which are in the Savannah-Greens Creek-Cullowhee area of Jackson 
County, the poorer grade of mica is near the footwall. 


Concentrations of mica are found in close proximity to walls and to inclusions of wall rocks at many 
mines. Zones near the walls commonly contain a higher proportion of plagioclase feldspar than the interior 
parts of the pegmatites. Where mica blocks occur in quantity along one wall but not the other, the hanging 
wall is generally favored. Mica streaks that occur both near walls and inclusions are found in the Caney 
Fork area of Jackson County. These pegmatites commonly contain tabular inclusions oriented parallel with 
the walls, and the pegmatite bodies, although irregular, generally conform to the foliation of their wall rocks. 
Examples of mines at which mica is localized near walls or inclusions are the Engle Cope (fig. 3), Lyle Knob 
(pi. 12), Shirley Wilson, Mack, Jeanie Deets, Aaron Hooper, Bud Williams, and Buzzard Roost. 

u See, for example: 
Olson, J. C, Mica-bearing pegmatites of New Hampshire: U. S. Geol. Survey Bull. 931-P, 1941, p. 375. 

Kesler, T. L., and Olson, J. C, Muscovite in the Spruce Pine district, N. C: U. S. Geol. Survey Bull. 936-A, 1942, p. 10. 
Cameron, E. N., Larrabee, D. M., et al., Structural and economic characteristics of New England mica deposits: U. S. 
Geol. Survey press bulletin, September 1944. 

Sylva District, North Carolina IS 


Granite bodies, discussed on page 10, are closely related to the mica-bearing pegmatites in at least 
five composite dikes. The granite bodies at the Big Ridge and Tilley mines are described on pages 28 and 54. 
The granite "cores" at the Moss, Borrows Cut, and Roarenhole mines occupy central positions within peg- 
matite masses, like the quartz cores of other pegmatites. Mica occurs in thin layers of coarse-grained peg- 
matite along the margins of the granite. It is uncertain at present whether the concentration of the mus- 
covite in the coarse-grained pegmatite was due to some effect of the granite, or whether the close spatial 
relation betwen muscovite and granite is only coincidental. 


The source of the pegmatite may best be considered by drawing a comparison with the Spruce Pine 
pegmatite district 100 miles to the northeast. The Franklin-Sylva district corresponds to the northwest 
half of the Spruce Pine district, inasmuch as it contains very little granite and the muscovite is dominantly 
rum or ruby in color and generally clear. The Cashiers district corresponds to the southeast half of the 
Spruce Pine district, which is characterized by much granite as well as muscovite that is characteristically 
green or brown and not uncommonly stained. The change in color of muscovite in different parts of the dis- 
tricts is very broad and general, and local exceptions are numerous. 

The granitic bodies in the Spruce Pine and Cashiers districts are coarse and pegmatitic, and are sur- 
rounded by shells of gneiss thoroughly permeated by granitic material. The granite of the Cashiers district 
probably contains more biotite and potash feldspar on the average than that at Spruce Pine. The main 
Franklin-Sylva pegmatite belt is separated from the granite masses of the Cashiers district by a relatively 
barren zone 5 to 10 miles wide in which there are very few mica-bearing pegmatites. (See pi. 1.) Similar, 
although much smaller, barren areas occur near the middle of the Spruce Pine district. The pegmatites at 
Spruce Pine are believed to have been derived from granitic rock whose present exposures lie mostly in the 
southeast part of the pegmatite district. 12 Similarly, the probable source of the Franklin-Sylva pegmatites 
is a granitic rock at depth, related to or part of the Whiteside granite masses of late Paleozoic age now ex- 
posed to the southeast in the Cashiers district (pi. 1). Apparently at the time of this granitic intrusion the 
pegmatites were emplaced in fractures and zones of weakness in the already folded and metamorphosed gneiss 
and schist. 

The minerals in the pegmatites that have formed in fractures appear to have been deposited essentially 
from the walls inward. This mode of formation is indicated by the fine-grained border zones, the cores of 
massive quartz that in many places have angular contacts with adjacent feldspar crystals, and the variation 
in content of microcline, plagioclase, and muscovite with relation to the walls, as described in preceding para- 
graphs. Most of the pegmatites are composed of relatively few minerals. Modification of the original peg- 
matite by later processes, such as albitization or large-scale replacement, is inconspicuous. 

The cores of the composite dikes, described on p. 10, are granite rather than quartz or another type 
of pegmatite. The granite at the Big Ridge mine occurs as the core, as part of the wall rock, and as dikes 
cutting both pegmatite and wall rock. The crystallization periods of granite and pegmatite here overlapped. 
The granite cores of the other composite dikes, like the quartz cores, probably solidified after the pegmatite 
along the walls, although the difference in age is probably slight. 



Muscovite is indispensable as an insulating material in certain types of electrical and radio equipment 
because of its unique combination of physical properties and our inability thus far to find a satisfactory 
substitute for certain uses. The most important physical properties in determining the value of sheet mica 
are cleavage, flexibility, staining, color, intergrowths with other minerals, and certain electrical properties. 
To be suitable for the most exacting uses, the mica must split readily into flat, clear, firm, flexible sheets, 
without staining, air or water bubbles, pinholes, or other inperfections. 

13 Olson, J. C, Economic geology of the Spruce Pine pegmatite district, North Carolina: North Carolina Dept. Cons, and 
Devel. Bull. 43, 1944. 

14 Mica Deposits op the Franklin- 

Muscovite crystallizes in the monoclinic system, and perfect crystals have nearly hexagonal outlines. 
Well-formed crystals are particularly common at the Tilley mine and occur sparsely in other pegmatites in 
the district, but by far the greater part of the commercial mica occurs as rough blocky masses of irregular 
shape. The largest mica block, or "book", reported from the Franklin-Sylva district was found in 1907 at 
the Iotla-Bradley (Iotla Bridge) mine. It weighed more than 4,000 pounds, and measured 4 feet in length 
or thickness 13 and 29 by 36 inches in cross-section. 

Certain physical peculiarities of "book" muscovite are of great economic importance. "A" mica is less 
valuable than flat, for the surfaces of the sheets are marred by chevron-like "reeves" or lines that intersect at 
an angle near 60 degrees, forming a "V". Some of the "A" structures are due to the tapering out of certain 
sheets along straight lines ; others are due to closely-spaced folds or corrugations, called "ridges" or "reeves", 
and mica possessing this feature is said to be "reeved". "A" mica occurs in variable proportions in most of 
the mines in the district, but is of minor quantitative importance at most mines. "A" mica from which flat 
mica can be obtained by trimming between the reeves is known as "flat A" mica. Mica crystals, mostly of 
"A" type, that taper in thickness are known as "wedge" mica. "Herringbone" mica differs from "A" mica 
in having two sets of reeves that intersect a central spine-like set at angles of about 60 degrees. Mica that 
tears when split, generally because of the intergrowth of adjacent sheets, is said to be "tanglesheet", "tied", 
"gummy", or "locked". Random fine cracks are known as "haircracks". "Ruled" mica is mica that is broken 
along sharply defined parting planes that intersect at angles near 60° and lie at an angle of nearly 67° with 
the cleavage plane. Ruling that is strongly developed in only one direction yields strips of "ribbon" mica. 
Ruling in two or three directions yields sheets of rhombic or triangular shape. Ruled mica results from 
distortion of the crystal by rock movements and is conspicuous near faults. The most productive sheet mica 
mines are therefore in pegmatites that have not been deformed. 

Intergrowths with other minerals impair the mica. The most common is that of muscovite with biotite, 
an intergrowth in which the cleavages of the two minerals are parallel. Although the presence of inter- 
grown biotite lowers the value of an individual muscovite book, the presence of biotite in a muscovite-bear- 
ing rock generally indicates that the muscovite is ruby or rum in color rather than green or stained. Other 
minerals intergrown with muscovite are quartz, plagioclase, flat and euhedral garnet, tourmaline, apatite, and 

The color of muscovite is denoted by the terms ruby (red or pink), rum (light-brown), green, white, and' 
dark-rum or brown. Staining of primary origin in mica is due to inclusions of hematite, magnetite, or tiny 
flakes of biotite. The type of staining due to small biotite flakes is rare but occurs in the Caney Fork area of 
Jackson County. The most common secondary stains are caused by the infiltration of fine clay particles be- 
tween the laminae and are called clay stains. Limonite commonly occurs as a result of the alteration of 
magnetite and hematite inclusions. Air and water bubbles occur between some sheets. If few, they can be 
removed by careful splitting, but if abundant they lower the value of the mica. 

The most important electrical property of mica is the power factor. Power factor, expressed in per- 
cent, is a measure of the loss of electrical energy in a condenser in which the mica forms the dielectric 
medium. Mica having a power factor greater than 0.04 percent is seldom used in condensers. The power 
factor of muscovite is greatly increased by the presence of such imperfections as staining, haircracks, pin- 
holes, and air bubbles. 


As the mica is taken from the mine, all that is obviously scrap because of physical defects or small size 
is segregated as "mine scrap" mica. The remaining mine-run mica is then split and trimmed ("rifted") 
in the mica shop. The products of the rifting process are sheet, punch or circle, and shop scrap. The common 
sizes into which sheet and punch mica are graded, and the approximate percentages of each size that have 
been produced from 12 outstanding mines during the period 1922-42, are shown in table III (page 18) 
which includes only mica classed as clear. Punch mica ordinarily includes clear sheet mica smaller than 1*4 
by 2 inches but larger than a circle 1*4 inches in diameter, and stained sheet mica smaller than 2 by 2 but 
larger than a circle l 1 /^ inches in diameter. The circle classification, as employed in the Franklin-Sylva dis- 
trict, ordinarily includes sheets ranging from a circle 2 inches in diameter to a 2 by 3 inch rectangle. During 

Sterrett, D. B., op. cit., p. 235. 

Sylva District, North Carolina 15 

the war, in accordance with increased demands for small mica, the minimum acceptable size for punch mica 
was lowered to 1 by 1 inch, and prices were based upon full and three-quarter trim, a higher standard of 
preparation than existed in pre-war years. 

Sheet mica is classified qualitatively into two primary divisions : "clear" and "stained". It may also 
be classified as No. 1, No. 2, or No. 3. No. 1 is clear mica of good quality, corresponding approximately to 
the Indian and A. S. T. M. grades of "clear", "clear and slightly stained", "fair-stained", and some "good- 
stained". No. 2 is less perfect because of curved cleavage, clay-staining, minor iron-oxide staining, or air 
bubbles; it corresponds to the Indian "stained" classification and possibly to some Indian "black-stained". 
No. 3 mica is heavily stained, like the Indian "black-stained or spotted" mica. The No. 2 mica has been 
further divided into "No. 2 regular" and "No. 2 inferior". In general the sizes and qualities in greatest 
demand during the war, and for which a premium price has been paid by the Colonial Mica Corporation, in- 
clude full-trimmed punch mica larger than 1 by 1 inch and full and three-quarter trimmed sheet mica IV2 by 
2 inches or larger, of No. 1 and No. 2 qualities. Prices, classification, and methods of preparation have varied 
during the war as well as in pre-war years, and the reader is referred to other publications 14 for further dis- 
cussions of the mica industry. 


The muscovite throughout the Franklin-Sylva district has a strikingly uniform rum to ruby color. On 
the average, mica from the northwest half of the belt has a slightly redder hue than that from the southeast. 
Mica from the parallel Cashiers district, 10 to 15 miles to the southeast, has a predominant dark-rum or 
greenish hue, and much of it is specked or stained. This type of mica is also common in the southeastern 
part of the Franklin-Sylva district, in the Wolf Mountain-Pinhook Gap area. Black-stained mica is rela- 
tively uncommon in the district, but staining caused by many minute biotite flakes in the mica is particularly 
common in the Caney Fork area of Jackson County. 

The quality of some of the mica in the Franklin-Sylva district is lowered by imperfections such as wavi- 
ness, mottling and surface stains, haircracks, tangle-sheet structure, and ruling. Ruling and waviness are 
related to the faults of small displacement that are widespread throughout the district. "A" structure is 
common in the Cashiers district. In the Franklin-Sylva district it is found at many localities but impairs 
far less mica than in some other 'domestic mica districts. Wedge "A" mica is abundant in several pegmatites 
near Greens Creek, Jackson County. 

No clearcut relation has been established between quality of mica and type of mica occurrence or shape 
of the enclosing pegmatite body. In general, the irregular pegmatite bodies that contain many tabular in- 
clusions of wall rock and only small or scattered quartz masses yield a lower percentage of high-quality sheet 
mica than the more sharply defined, discordant dikes that have well-developed quartz cores. Pegmatites 
mined predominantly for scrap mica are represented among the large irregular masses — for example the 
Iotla-Bradley, Berry, Burr Knob, Big Flint, Annie Laurie, and in large part the Shepherd Knob. Likewise, 
pegmatite bodies with similar structures in the Caney Fork area have yielded dark-colored mica that is com- 
monly stained. 



Pegmatite mining in the district began with the production of kaolin by the Cherokee Indians, presum- 
ably for shipment to England. As early as 1744, an English patent was recorded for the production of 
porcelain from an earthy mixture produced by the Cherokee Nation in America, consisting probably of kaolin, 

14 See, for example: 

Wierum, H. F., and others, The mica industry: U. S. Tariff Commission, Rept. 130, 2nd ser., 1938. 

A. S. T. M., Grading and classification of natural mica: Amer. Soc. for Testing Mater., Release D-351-38, 1938. 

War Production Board mica releases No. 1 and No. 2, July 6, 1942. 

Gwinn, G. R., Strategic mica: U. S. Bur. Mines Inf. Circ. 7258, 1943. 

Wayland, R. G., Mica in war: Mining Technology, vol. 8, no. 4, July, 1944. 

Billings, M. H., and Montague, S. A., The wartime problem of mica supply; Eng. and Min. Jour., vol. 145, no. 8, pp. 92-95, 

Lintner, E. J., Mica, a war essential mineral: Rock Products, vol. 47, no. 5, pp. 48-50, 92-93; no. 6, pp. 74-76, 114-116, 1944. 

16 Mica Deposits of the Franklin- 

feldspar, and quartz. 15 Thomas Griffiths came to the Cowee section of Macon County from England to ob- 
tain kaolin in 1767. 16 He cleaned out an old pit from which kaolin had been extracted previously, and trans- 
ported at least 5 tons of the kaolin to Charleston for shipment to England. Modern kaolin mining in North 
Carolina began about 1888 near Webster, in Jackson County. For a number of years the production was 
largely from the Franklin-Sylva district, and was small, but about 1900 North Carolina began to gain promi- 
nence as a kaolin-producing state. In recent years, North Carolina's entire output has been from the larger 
deposits in the Spruce Pine district. 

Mica is believed to have been mined by the early Indians presumably for ornamental purposes. Re- 
mains of extensive workings of ancient origin are reported to have been found at the Baird mine. 17 
Sterrett 18 summarizes the beginnings of mica mining as follows : "Modern mica mining in North Carolina 
was begun in 1867 by L. E. Persons, of Philadelphia, previously of Vermont. Mr. Persons' attention was 
directed to Jackson County by someone in Philadelphia who had seen a mica crystal exhibited at the State fair 
in Columbia, S. C, in 1858, by D. D. Davies, of Webster. In the autumn of 1867, Mr. Persons went to Jack- 
son County and learned from Mr. Davies the location of favorable prospects for mica in Jackson and Hay- 
wood Counties, which he soon opened." The Big Ridge mine is generally considered to be the first mica mine 
to be developed in the district. 


The weathered near-surface parts of pegmatites are mined first by pick-and-shovel open-cut methods, 
although in some places steam shovels, drag lines, bulldozers, and hydraulic methods have been used in soft 
material. Timbering is ordinarily necessary as soon as underground work is begun, as workings cave easily. 
The deeper mines encounter hard rock that must be drilled and blasted. Barren rock is not broken unless 
absolutely necessary ; hence, many openings are narrow and tortuous. 

The pegmatite mining is for mica almost exclusively, although many mines were first developed for 
kaolin, and the principal product at the Sally Reed, Lin McCall, McGuire, and Doc Sanders mines has been 
feldspar. As a general rule, only one pegmatite body is mined at any one mine. The largest workings for 
sheet mica are those at the Big Ridge mine, described on page 28. Some mines have been very productive 
although the sizes of their openings are small — for example, the Moody, described on page 42, and the 
Beasley No. 1, described on pages 20-22. Doubtless unusually rich mica shoots were mined from these two 


In the average sheet-mica mining operation, from 5 to 15 tons of rock are moved daily, yielding a few to 
500 pounds of mine-run mica. The largest sheet-mica operation in 1942, the Big Ridge mine, yielded about 
2,300 pounds of mine-run mica daily, while 29 tons of waste rock were moved to the dump during a 14-man 
10-hour shift. Inasmuch as some muck or waste was also left in the mine on lofts, the mine-run mica evi- 
dently constituted between 3 and 4 percent of the total pegmatite mined. Additional figures on more recent 
output of the Big Ridge mine are given on page 32. 

Total mica in the rock mined probably ranges from 3 to 10 percent at most good mica mines, but if mine 
scrap and mica too small to be recovered are excluded, the mine-run mica probably ranges from about one to 
four percent of the rock mined. The decomposed pegmatites at the Iotla-Bradley and Shepherd Knob mines 
are estimated to be 10 to 12 percent muscovite, but their content of scrap mica is exceptionally large. The 
output of a typical sheet-mica mine, under pre-war conditions which permitted the inclusions of much low- 
grade material in the sheet and punch mica, consisted of about 80 percent scrap, 15 to 16 percent punch, and 
4 to 5 percent sheet mica. Different standards of quality and preparation during the war have brought about 
a diminution in the percentages of sheet and punch mica recovered. Table III shows the proportions of punch, 
circle, and various sizes of sheet in nearly 2,000,000 pounds of mica produced from 12 mica mines in the 
Franklin-Sylva district during the period 1922-42, and similar figures for the Big Ridge mine. These indi- 
cate what sizes might be expected in the future from the better mines in the district. Scrap mica generally 
averages 65 to 95 percent of the total mica produced. 

15 Watts, A. S., Mining and treatment of feldspar and kaolin in the Southern Appalachian region: U. S. Bur. Mines Bull. 

53, p. 10, 1913. 
18 Ceramic Age, vol. 14, no. 5, pp. 165-169, November 1929. 

17 Smith, C. D., Ancient mica mine in North Carolina: Smithsonian Inst. Rept., pp. 441-443, 1876. 

18 Sterrett, D. B., op. cit., p. 167. 

Sylva District, North Carolina 17 

The proportion of high-quality sheet and punch mica to the total mine run has become increasingly im- 
portant as a factor in mining, because of the increased demand for such qualities during the war. The mica 
is classified quantitatively according to percentages of No. 1, No. 2, "No. 2 inferior", and No. 3 grades. The 
proportion of Nos. 1, 2, and "2 inferior" to the total mine run averages only a few percent, rarely exceeding 
12 percent, but upon this ratio depends to a great extent the value of the total mine-run mica. 


Scrap mica is obtained in the Franklin-Sylva district both as a by-product from sheet-mica mining and 
from decomposed pegmatite mined chiefly for scrap mica by pick-and-shovel, power shovel, or drag-line 
methods. In 1942, three plants for recovery of scrap mica were in operation near Franklin, utilizing ma- 
terial from large open cuts in weathered pegmatite and from dumps of previous sheet mica mining opera- 
tions. In 1944 scrap mica was being produced by the following concerns : 

(1) Bradley Mining Company, and (2) Duvall and Liner, both at Iotla Bridge on the Little Tennes- 
see River. 

(3) Fred Arnold (Arnold Mines) plant about one mile southeast of Iotla Bridge, on the Little Ten- 
nessee River. 

(4) The Franklin Mineral Products Company mica grinding plant in Franklin. 

The feed for the several scrap mica washing plants is either decomposed pegmatite or dump material 
from old mica mines. The decomposed pegmatite used in the summer of 1944 was mined from the Iotla- 
Bradley and Shepherd Knob pegmatites, and is reported to have averaged about 10 percent muscovite. The 
large pegmatites rich in small mica have been best suited to this purpose — for example the Shepherd Knob 
(pi. 17), Iotla-Bradley (p. 37), Berry, and Big Flint (p. 26). 


In the Franklin-Sylva pegmatites feldspar is at present the only mineral of commercial value other than 
mica. The relatively low price of crude feldspar does not permit profitable production where mining or 
transportation costs are high ; accessibility and haulage facilities are more significant economic factors than 
in mica mining. Feldspar mining has seldom been profitable in the Franklin-Sylva district because of the 
low unit value (about $6 to $7.50 per ton) and the high cost of transportation to the nearest market at 
Spruce Pine, about 100 miles distant. Pegmatites suitable for feldspar mining are more sparsely distributed 
in the Franklin-Sylva district than at Spruce Pine, but coarse potash feldspar is abundant in some pegma- 
tites, particularly several in the Pinhook Gap-Wolf Mountain area of Jackson County. 

Feldspar has been produced since about 1933 near Bryson City, in Swain County, adjoining the Franklin- 
Sylva district on the northwest. Prior to the summer of 1945 this feldspar had been shipped to Spruce 
Pine either by rail or truck. In the fall of 1945 a feldspar grinding mill was put into operation at Dillsboro 
and plans were under way for the construction of another at Bryson City. 


Reliable and complete production figures for the Franklin-Sylva district are not available for years 
prior to 1942. Minerals Yearbook 19 lists the annual production of combined sheet and punch mica for the 
State of North Carolina, shown in Table II for the period 1920-44. Purchase records of the Asheville Mica 
Company, buyers of nearly all of the mica in the district, were also consulted and provided the most accurate 
basis for estimating the amount of mica produced by the district during the period 1922-42. During this 
period, sales of mica were made from more than 75 mines ; a summary of the approximate total production 
of 12 of the mines for which the records are most complete is shown in Table III. 

The 12 mines whose production is shown in Table III produced most but by no means all of the mica 
from the district during the years 1922-42, for at least 75 mines were active at times during this period. 
The total for the 12 mines, 1,998,266 pounds of sheet and punch mica, can be compared with the State's 
total for a similar 21-year period 1920-40, for which production figures are available. During the period 
1920-40 North Carolina's output amounted to 13,263,462 pounds of sheet and punch mica, valued at $2,557,511 
(table II). From these figures it is estimated that the annual production of sheet and punch mica in the 
Franklin-Sylva district during the period 1920-40 was nearly 20 percent of the total for the State, or nearly 
126,000 pounds of sheet and punch mica annually. Most of the remainder of North Carolina's output, prob- 
ably about 75 percent of the total, has been obtained from the Spruce Pine district. 

U. S. Bur. Mines, Minerals Yearbook. 


Mica Deposits of the Franklin- 

table ii 

Recorded Production 20 of Sheet and Punch Mica from North Carolina, 
Year Amount (Pounds) 






















































20 U. S. Bur. Mines, Minerals Yearbook. 


Approximate Production of Sheet and Punch Mica from the Big Ridge and 11 Other 

Mines in the Franklin-Sylva District, 1922-42 

Size of sheet 

Big Ridge mine 21 

12 of the principal producers 
including Big Ridge 



Percent of 
total sheet 


Percent of 
total sheet 

8 x 10- 

6 x 8 




















4 65 

4 x 6 

3 x 5 

3 x 4 

3 x 3 

8 32 

2 x 3 

23 45 

2 x 2 

20 53 

iy 2 x 2.... 

34 73 

Unclassified sheet 


Total sheet 


Percent of 

total sheet, 

circle, and 







Percent of 

total sheet, 

circle, and 


25 56 

Total punch 

68 69 

Total circle 

5 75 

Total sheet, 
circle, and punch 





21 Published by permission of K. A. Sprague, Haywood Lumber and Mining Company. 

Sylva District, North Carolina 19 

Production of high-quality mica under conditions of heavy demand and intensive mining activity during 
the war years, 1943-1944, is shown in Table IV. The amounts shown for 1942-44 cannot be compared di- 
rectly with the figures for previous years because of the differences in quality of preparation and grading. 
The pre-1942 data apply to half -trimmed sheet mica (1^2 by 2 inches and larger), both clear and stained, 
and untrimmed punch (1V4 inches in diameter). The mica sold to Colonial Mica Corporation since 1942 has 
been three-quarter trimmed and full-trimmed sheet (IV2 by 2 inches and larger) and full-trimmed punch 
(1 by 1 inches and larger) of No. 1 and No. 2 qualities, which exclude much heavily-stained mica. 


The history of past production of the district is the most reliable basis from which to estimate possi- 
bilities of future production. The average annual production during the years 1920-40 is estimated to be 
nearly 126,000 pounds of sheet and punch mica of all qualities. The monthly average of 10,500 pounds of 
high-quality sheet and punch mica during the last half of 1944 (see table IV) indicates the potentialities of 
the district under intensive development. This rate of production could probably be maintained for at least 
several years by the continued operation of productive mines and the development of other prospects as the 

table IV 

Production of Mica of Qualities Acceptable by Colonial Mica Corporation 
in the Franklin-Sylva District, 1943-44 22 

Period Pounds Sheet 

Oct.-Dec. 1943 24,578.49 

Jan.-June 1944 51,599.79 

July-Dec. 1944 63,004.62 

Total Oct. 1943-Dec. 1944 139,182.90 

23 Published by permission of Colonial Mica Corporation. 

more productive mines become depleted. An increase would probably result from the development of addi- 
tional headings at some of the better mines. 



J. M. Parker III 

The Allman Cove group of mines is 1^4 miles northwest of the center of the town of Franklin, in the 
east-central part of the Franklin quadrangle. The mines lie on low ridges west of North Carolina Highway 
28, from which they are easily reached over half a mile of good dirt road. The group includes the Allman 
Cove mine, the Mudhole mine, and the Willis mine. 

The earliest work at the Allman Cove mine was done about 1870 or 1880. Surface mining was done 
and a long adit was driven northward from the creek. (See pi. 3.) About 1904, the large pit at the west 
end of the workings was worked for kaolin to a depth of about 60 feet. The mine has been worked intermit- 
tently by many operators. Mica suitable for condensers and telephone equipment is reported to have been 
produced in 1918 or 1919. Since 1925 operations have been nearly continuous and have been carried on 
mainly by John and W. P. Brindle, John and Floyd Tallent, and J. W. Roper. The mine was worked be- 
tween January and March 1943 by F. E. Snow and E. B. Ward, and then until the summer of 1943 by Mr. 

The Mudhole mine was first explored about 1930 by John Tallent. The last operation, by Tallent and 
Roper, was abandoned in 1942 when the shaft became dangerous and the volume of water became difficult 
to handle. 

The Willis mine was worked first by Fred Willis, about 1926, and more recently by John Tallent and 
Ivy Crisp, the present owner. In July 1943, F. E. Snow drove a tunnel westward along the dike below the 
earlier workings. 

The Allman Cove mine consists of three large and several small pits, at least 16 shafts ranging in depth 
from about 15 to 90 feet, and many short drifts at various levels. The underground workings are now in- 
accessible, except the deep shaft and stopes at the east end. It is judged from reports that the pegmatite 
may have been almost completely worked out down to water level, which is 50 to 70 feet below the surface, 
a little above the altitude of the creek to the south. 

The pegmatite body is nearly divided into two parts by a projection of wall rock (mica gneiss) near the 
middle of the workings. The pegmatite body thickens both east and west of this point. The eastern part 
trends east and is nearly vertical. In the easternmost shaft the pegmatite is only 18 inches thick, but it is 
nearly 30 feet thick in the main workings, and about 20 feet thick in the large pit. The west part of the 
pegmatite trends N.70°W. and probably dips steeply to the south. It is about 20 feet thick and probably 
tapers out at the southeast end and branches into several stringers at the northwest end. The pegmatite is 
intrusive into mica gneiss ; in general it lies parallel to the strike of the foliation but in places cuts across it. 

The pegmatite is composed of partly kaolinized feldspar (probably plagioclase), quartz, muscovite, and 
biotite. The eastern part of the pegmatite contains a number of irregular streaks of "burr rock", which has 
been described on page 9. All of the mica seen in the east workings was small, wavy, ruled, and cracked. 
Most of it was scrap but a little would yield punch or sheet up to about 2 by 2 inches. The mica was moder- 
ately stained by clay and iron oxide, and intergrowths with biotite were abundant. 

The underground workings at the west end were flooded and could not be examined ; hence the following 
description of this part of the pegmatite is based upon reports by miners. A well-defined quartz mass, 2 to 
at least 3 feet thick, in part "burr rock", lies in the middle of the pegmatite body. Sheet mica has been 
found on both sides of it, but most of the mica is along the south wall. The mica occurs in larger books at 
this end than at the east, but it is considerably ruled. Flat, hard, clear, dark-rum mica is produced. Very 
little biotite is found. 


M. R. Klepper and J. C. Olson 

The first work at the Beasley No. 1 mine is reported to have been done in the main open cut about 1880 
or 1885. A large amount of mica is said to have been mined from an unusually rich pegmatite vein during a 
period of several years. The old dumps were later reworked for scrap mica. After many years of idleness, 

Sylva District, North Carolina 



(Dota from F. E. Snow) 

1926' Level 

— 2000 


— I960 

— 1940 


area shown on 
underground maps 

Scale in feet 
Contour interval 10 feet 

Datum assumed 



Pegmatite, undivided 

Scrap mica 

Quartz- muscovite pegmatite ("burr"] 

Mica gneiss 

"eo Contact, showing dip 

Contact, approximate 

'' Trace of pegmatite body 


^ Outline of underground workings 


B Shaft, showing depth in feet 

a Foot of raise 
to Rim of open cut 

Mapped by J M.Parker III ond V.'C.Fryklund, Jr. June- July 1943 

Map and Sections of the Airman Cove Mine, Macon County. 

22 Mica Deposits of the Franklin- 

the mine was leased in June 1943, to the Thurman Mining Company, which developed all of the west open- 
cut. This operation was abandoned about the end of April 1944. 

The country rock is garnetif erous biotite gneiss with some layers of quartzose mica gneiss. The foliation 
strikes N.65°E. on the average and dips 25°N. to vertical. Steep southerly dips occur at several places in the 
southern part of the area. The change from northerly to southerly dips takes place near the main pegmatite 
vein; within a few feet of the contacts the gneiss is severely contorted and contains much pegmatitic or 
granitic material. The pegmatite evidently was emplaced in a fault or zone of sharp folding. A vertical 
pegmatite 3 inches thick, which is exposed in the stripped area above the west open-cut, sharply cross-cuts 
the foliation of the gneiss. It was probably emplaced in a fracture. 

The main open cut and the west cut (pi. 4) are in different pegmatite bodies. Both pegmatites are very 
irregular, with general easterly strikes and southerly dips. Pegmatite offshoots that extend into the wall 
rocks are both discordant and conformable with the foliation. 

Pegmatite in west cut. — The pegmatite in the west cut strikes east and dips 55°S. From a maximum 
thickness of 12 feet in the face, it pinches upward and eastward to about a foot at the edge of the cut, where 
it consists mostly of quartz. It is made up of three principal rock types. (1) Oligoclase-rich pegmatite, con- 
taining biotite, muscovite, quartz, and garnet, occurs in zones 1 to 4 feet thick adjacent to each wall of the 
pegmatite body. (2) Quartzose pegmatite occurs within the oligoclase zones as layers 1 to 7 feet thick. 
(3) Muscovite-rich pegmatite occurs in a zone about 2 feet thick in the center of the pegmatite, and less 
prominently near the hanging wall. 

Biotite is relatively abundant in part of the oligoclase pegmatite near the footwall and with muscovite 
and quartz in the central part of the pegmatite. Pyrrhotite and apatite are also present. 

Most mica in the west cut is clear ruby, but a little is green. Most of the green mica is black-specked, 
reeved, warped, and broken. Some of the ruby mica is lightly specked, but most is clear. The principal de- 
fects are "A" structure, warping, and ruling. 

Pegmatite in main cut. — The main pegmatite body is one-half to one foot thick at the west end of the 
main cut, but thickens eastward. The part of the pegmatite that is 5 feet or more thick has a strike length 
of about 100 feet ; it swells to more than 15 feet in thickness midway along this length. The dip is steep in 
the open cut, but decreases southward in the stope to less than 45°. Many who know the history of the mine 
describe the pegmatite as an unusually rich "pocket", suggesting that the pegmatite thins down-dip as well 
as along the strike. 

Only a thin rind remains along each wall of the pegmatite in the main cut. This zone is very rich in 
scrap mica, especially along the hanging wall. Almost all the mica books are less than 2 inches in diameter, 
and are interlocked in pegmatite that also contains a little oligoclase and quartz. The core of the pegmatite, 
near the middle of the open cut, is reported to have been a thick mass of quartz. Mica is reported to have 
been unusually abundant along the margins of the central quartz body. This quartz mass was thickest in the 
part of the pegmatite at the middle of the main open cut, and thinned out to the east and west. Near the east 
end of the area, the pegmatite feathers out into several narrow stringers that contain only scrap mica. Other 
offshoots extend westward from the main cut. Two of these are very rich in scrap mica; one has been ex- 
plored by the adit and the other, which is 1 foot thick, is exposed at the west end of the cut. 

Mica from the main cut was probably of better quality than that from the west cut. It is mostly clear 
ruby. Although "A" structure and other physical defects are present, they are not as prominent as in mica 
from the west cut. Very little biotite occurs in the main pegmatite. 


M. R. Klepper and E. Wm. Heinrich 

The Beasley No. 2 mine is 8 airline miles N.25°E. of Franklin. It lies near the head of an unnamed 
branch on the north side of Caler Fork Valley, at an altitude of 3,150 feet. The mine is reported to have 
been operated by the Bowers brothers of Franklin in 1890, and has been worked intermittently up to the 
present time. It is owned by the Masonic Lodge of Franklin, who leased it in the summer of 1942 to the 
Asheville Mica Company of Biltmore, N. C. Operations were begun on September 1, 1942. 

Sylva District, North Carolina 








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24 Mica Deposits of the Franklin- 

The old workings consist of 8 surface cuts, a shaft caved at a depth of 13 feet, an inaccessible inclined 
shaft, an adit caved 40 feet from the portal (Adit C), and another adit (Adit B) that opens into drifts and 
stopes. (See pi. 5.) The stopes, now accessible only in their lower parts, were first worked from the in- 
clined shaft and later connected with Adit B. From September 1942, to May 1943, the pegmatite body was 
mined in the drift and stopes from Adit B. Adit A was begun in May 1943, and reached the pegmatite in 
June. By May 1944, overhand stopes from this adit had been connected with underhand stopes from Adit B. 

The country rock is banded biotite gneiss. In the northern part of the area the foliation strikes a few 
degrees north of east and dips steeply north. The foliation of the rock in the southern part of the area has a 
similar strike but dips to the south. These relations suggest a tightly folded anticlinal structure, the axis of 
which trends nearly east. The pegmatite body strikes a few degrees north of west and dips on the average 
45°SW. It has been explored over a strike length of 370 feet and over a vertical distance of 250 feet. The 
thickness ranges from 21/2 to 12 feet, with an average of 8 feet. 

Some parts of the pegmatite body are well zoned. An average section from hanging wall to footwall in 
the zoned part of the pegmatite is as follows : 

Pegmatite Thickness 

Medium-grained quartz-feldspar 

pegmatite ; no muscovite 6" to 1' 

Pegmatite rich in coarse muscovite; 

remainder chiefly feldspar (plagioclase?) 1' to l 1 /^ 

Coarse plagioclase, with very little 

quartz or muscovite 2' to 2y 2 ' 

Muscovite-biotite selvage 3" to 6" 

Massive quartz 3' to 4' 

Medium-grained quartz-feldspar pegmatite 

locally containing small books of muscovite 6" to 1' 

The quartz core, which plunges southeast at an angle of about 35°, has a horizontal width of about 120 
feet. The core and the accompanying muscovite zone are absent from the exposures in the surface cuts and 
the higher accessible parts of the stopes. Here a rough three-fold layering is present; a narrow selvage of 
barren quartz-feldspar rock occurs along both walls, and the remainder is plagioclase-rich pegmatite that con- 
tains biotite and muscovite. 

West of the end of the quartz core on Level Z (pi. 5, underground map) the drift passes through a 25- 
foot zone of hybrid pegmatite which contains numerous inclusions and septa of biotite gneiss. Beyond this 
zone of hybrid pegmatite the body contains a core of very coarse-grained quartz and feldspar and a rudi- 
mentary muscovite zone near the hanging wall. The quartz core also ends near the eastern face of Level Y. 
Between the end of the quartz core and this face the pegmatite body thins from 7 to 2y 2 feet, and it may 
possibly pinch out toward the east. 

Muscovite occurs in a well-defined zone between the barren hanging-wall rind and the zone of coarse 
plagioclase. A thin selvage of muscovite with biotite lies along the hanging-wall side of the quartz core, 
but this mica is too severely broken to be of strategic value. The lateral extent of the mica zone appears to 
coincide with that of the quartz core, and both the mica shoot and the core plunge about 35° southeast. Mica 
books are as much as 2 feet wide and 3 inches thick ; ribbons 16 inches long and 5 inches wide were also noted. 
Ruling, warping, and cracks are the principal defects ; "A" structure and mineral inclusions are subordinate. 
The mica is deep rum and the books are generally hard and flat. Much of it is of very good quality. Flat 
sheets measuring 6 by 8 inches were trimmed from some of the larger books. 

The following estimates and calculations are for the period between December 27, 1943, and May 26, 1944 : 

Total pegmatite mined 1200 tons 

Pegmatite mined per average day 9 tons 

Mine-run mica produced per average day 400 pounds 

Percentage mica in pegmatite* J 2.2% 

Total mine-run mica produced 25.5 tons 

Total No. 1 and No. 2 sheet and punch mica 

produced** 6000 pounds 

Percentage of No. 1 and No. 2 sheet and punch 

mica in mine-run, calculated 12 % 

Percentage No. 1 and No. 2 sheet and punch 

mica in mine-run, estimated average 8% 

•Allowing for loss on dumps. 
♦♦Probably includes some mica produced before December 27 and sold after that date. 

Sylva District, North Carolina 




1 1 1 





o o O 

■O IO ft 



























26 Mica Deposits of the Franklin- 


E. Wm. Heinrich 

The Big Flint mine, also known as the Grassy Ridge mine, is 2 airline miles S.57°E. of Balsam, Jackson 
County. The mine lies 200 feet above and 300 feet northwest of the northern branch of Cabin Creek on the 
southeast flank of Grassy Ridge, and about half a mile southwest of the Haywood County line. The property 
is owned by the heirs of the Tom Lee Estate of Waynesville. W. W. Davis of Waynesville leased the pro- 
perty in 1932 and operated it as a scrap-mica mine until August 1942. A scrap plant, consisting of bins, two 
crushers, conveyor flumes, and a dryer, was constructed. In August 1942 Davis sold out to the Balsam Min- 
ing and Milling Company, which operated the mine for both sheet and scrap mica until December 15, 1943. 
Fred Lewis of Hazelwood secured the lease on March 1, 1944, and attempted to operate the property for 
sheet mica and washer stock. This operation did not prove successful and Mr. Lewis ceased work early in 
May 1944. 

Surface workings (pi. 6) consist of three large irregular open-cuts arranged along a line that trends 
N.65°E. The underground workings consist of three adits, a level of irregular drifts and crosscuts, several 
large stopes, and several winzes and raises. Adit A was worked by Fred Lewis ; all the other workings are 
old, and were dug either during or before the period of operation by W. W. Davis. 

The country rock is a fine-grained, locally garnetiferous, biotite gneiss. It is conspicuously contorted, 
especially near contacts with the pegmatite mass. The rock has been intruded by a very large body of peg- 
matite with a minimum width of 300 feet and an explored strike length of 375 feet. The northwestern con- 
tact of the body, which is well exposed, has a general trend of N.60°E. In Cuts I and II the contact has a 
general steep dip to the southwest, but in Cut III it is reversed to steeply southeast. Along the southwestern 
wall of Cut III are exposed several thick bands of gneiss, which suggest a proximity to the southwestern con- 
tact. In general the pegmatite body cuts across the foliation of the gneiss. 

The pegmatite body contains a large body of massive quartz which forms a prominent white outcrop be- 
tween the two northern cuts. The quartz body widens toward the southwest and ranges in thickness from a 
few feet to 65 feet. It is 130 feet long, is exposed over a vertical distance of 85 feet, strikes N.45°E., and 
dips steeply northwest. At its northeastern end 4 feet of barren pegmatite separates the mass from the 
northwestern contact with the gneiss ; in the northwestern arm of Level D the quartz body is in contact with 
the gneiss, but at the southwest end of the mass 45 feet of pegmatite lies between it and the gneiss. 

Along the footwall of the quartz body is an unusual mineralogic zone consisting of innumerable sub- 
parallel and shard-like slabs of quartz, which range in thickness from a fraction of an inch to nearly a foot 
and are separated from one another by films of biotite that give to the rock a strongly foliated appearance. 
Generally the slabs and films are parallel with the footwall of the quartz body. 

The bulk of the pegmatite body is a medium-grained aggregate of quartz, feldspar, muscovite, and biotite. 
Although some of the biotite occurs in thin strips as much as 3 feet long, the percentage of biotite in the body 
as a whole is low. Most of the muscovite occurs in small flakes and books rarely over 1 inch in diameter. 
Both microcline and plagioclase are present and the latter is generally more kaolinized. Plagioclase appears 
to be the more common feldspar near the northwest contact, but in the central part of the pegmatite micro- 
cline is more abundant. 

Two well-defined zones of coarse mica occur in the pegmatite body, one along the footwall contact of the 
quartz mass and the other along the northwestern contact with the gneiss. The quartz footwall zone has been 
extensively mined in the underground workings. It has a maximum thickness of 3 feet, and books of mica 
as much as 5 inches in diameter have been observed in it. This zone appears to be very persistent and the 
quantity of mica obtained from it appears to have been large. The zone along the northwest contact with the. 
gneiss was mined in Adit A. This zone is discontinuous and consists of scattered concentrations of mica over 
a width of 7 feet. Books as much as 9 inches in diameter were obtained from this zone. 

The principal defects of the mica are closely-spaced ruling, persistent and through-going fractures, a 
light-green mottling, and dark spots and minute inclusions of biotite. Because of the cracks and ruling, even 
the largest books will yield only small sheets or punch. 

The mine has been a large producer of scrap mica and considerable quantities of pegmatite rich in scrap 
mica remain to be mined. The richest concentrations of scrap mica occur in a belt that is parallel to the 

Sylva District, North Carolina 




1 A 



2j 1 



^\ J v vf 









Scole in feel 
Contour Intervol ten feet 
Ootum from U.S.G.S Cowee Quadrangle 

ftonttable survey Mapped by E.wm.Heinrteh, MR.Ktepper, ond L-C.Pray April 1944 
Revised by E-Wm.Heinrich March 1945 



Qucrtz-biotite pegmatite 


Muscovite pegmatite 


Quorlz-plogioclose pegmatite 


Quartz- plagioclose-muscovite pegmatite 


Coarse microcline 


Mossive quortz 


Biotite gneiss 


Contact wiln dip 


Approximate contact 


Contact between pegmatite units 


Attitude of pegmatite ploty structure 



Attitude of foliation 

Limit of exposure 


Rim of open cut 


Foot of dump 


Outline of adits 

Outline of Level and Slope E - 

Map and Sections of the Big Flint Mine, Jackson County. 

28 Mica Deposits op the Franklin- 

trend of the pegmatite body and has a width of about 80 feet along the northwest side of the mass. This belt 
is estimated to contain between 5 and 10 percent of scrap mica. Beyond this width the content of scrap mica 
is markedly less. The transition to the scrap-poor part seems to be accompanied by an increase in the per- 
centage of microcline. 


M. R. Klepper and E. Wm. Heinrich 

The Big Ridge mine is 3.9 airline miles S.21°E. of Hazelwood, Haywood County. It lies on the south- 
west slope of Roberson Ridge on a rounded nose between two unnamed branches of Deep Gap Creek. Most of 
the workings are at altitudes between 4,500 and 4,700 feet. The Big Ridge mine is believed to be the oldest 
mica mine in North Carolina on the basis of continuous operation. From 1922 to 1944 it yielded at least 
436,000 pounds of sheet mica and 807,000 pounds of punch mica. 

The first prospect pits are reported to have been dug near the old caved shaft. (See pis. 7 and 8.) 
In 1915 J. E. Burleson began the lower adit ; by 1944 it had been advanced to a length of 1,060 feet and had 
been stoped over 650 feet of this length. The mine is owned by the Haywood Lumber and Mining Company 
of Waynesville, and for the last ten years it has been under lease to T. L. Blalock of Hazelwood. 

The Big Ridge pegmatite body is an irregular dome-shaped intrusive, the long axis of which trends 
N.55°E. The body has been mined from a series of interconnected drifts, stopes, and chambers over a length 
of 650 feet, and over a maximum width of 300 feet. The vertical extent of the workings is 200 feet. This 
maze of workings is oval in plan and asymmetrically arch-shaped in both longitudinal and tranverse sections. 
(See pi. 8.) 

The top of the pegmatite dome (fig. 2) is nearly flat with a shallow elongate central depression parallel 
to the long axis of the dome. Distinct ridges border this central depression. The general domal shape of the 
mass is interrupted by numerous apophyses, which project upward from the top, and by a large off -shoot 
from the southwest side. At the southwest end of the workings the top of the dome narrows and plunges 
steeply southwest. For about 200 feet east of this steeply plunging nose the upper half of the south flank of 
the dome dips to the northwest and the lower half is vertical or dips steeply southeast. (See pi. 8.) Toward 
the east the dip of the south flank becomes vertical, then gradually changes to steeply south, and finally to 
moderately south. The dip of the northwest flank of the dome decreases from about 70 °W. at the nose to 
about 30°NW. near the northern end of the workings. 

The thickness of the pegmatite ranges from 2 to 25 feet. It is thickest around the steeply plunging nose 
and the marginal ridges of the top, and thins along the flanks, except at junctions with apophyses. The hang- 
ing-wall contact along the northwest flank of the dome is step-like in structure, consisting of alternating 
steeply dipping "risers" and nearly horizontal "treads". 

The main rock types that occur are biotite gneiss, pegmatite, granite, and a felsitic dike rock. In addi- 
tion, gradational or hybrid rock types occur between pegmatite and gneiss, pegmatite and granite, and gneiss 
and granite. The gneiss, into which the pegmatite has been intruded, consists of fine- to medium-grained 
quartz, biotite, and a little garnet. It occurs chiefly along the outer contact of the pegmatite. The foliation 
strikes northwest and dips southwest. The pegmatite is simple in mineral composition, containing plagio- 
clase, quartz, biotite, and muscovite, with very minor quantities of microcline. The accessory minerals are 
apatite, pyrrhotite, ankerite, and hedenbergite. Except for concentrations and zones of mica-rich pegmatite, 
the mass as a whole is very poorly differentiated. Small discontinuous quartz lenses were observed in only 
two places. The order of abundance of the minerals in the pegmatite is estimated to be : plagioclase 73 % ; 
quartz 20% ; muscovite 3% ; biotite 3% ; others 1%. The main mass of pegmatite consists of a coarse- 
grained intergrowth of plagioclase, quartz, biotite, and muscovite. The proportion of biotite varies widely 
and sheets of the mineral are locally arranged perpendicular to the contacts with the gneiss. 

The granite is a uniformly medium-grained rock consisting of gray plagioclase, biotite, muscovite, and 
quartz, in that order of abundance. The rock has a slight foliation due to the orientation of biotite flakes, but 
the percentage of biotite varies widely. The granite occurs as discontinuous masses along the inner margin 
of the pegmatite mined, which in most places is the footwall. Small pods and lenses of granite also occur 
locally within the pegmatite body itself. The largest body of granite, which occurs below the nose of the 

Sylva District, North Carolina 













I— c 






Mica Deposits of the Franklin- 

Fig. 2. — Structure Contours on Top of Pegmatite Body, Big Ridge 

Mine, Haywood County. 

pegmatite, is known to have a vertical extent of 100 feet and a thickness of at least 60 feet. This mass 
appears to thin along both flanks of the pegmatite, but the exact footwall contact of the granite with the 
gneiss is nowhere exposed. The pegmatite and the granite appear to be closely associated in origin, as 
transitional rock types between the two were observed. Large crystals of plagioclase, biotite, muscovite, 
and apatite lie entirely within the granite or extend across contacts between the two rocks. In general, how- 
ever, contacts between these rocks are sharp, and locally small tabular dikes of granite cut across the peg- 
matite body. The crystallization periods of the granite and the pegmatite apparently overlapped. 

The youngest rock in the deposit is a felsite, which occurs in tabular dikes, as much as 6 inches thick, 
transecting both pegmatite and gneiss. 

The quantity of mica in the pegmatite varies considerably in different parts of the mine. In general the 
best concentrations of mica have been found where the pegmatite is underlain by granite. Pegmatite around 
the nose of the body and along the southwestern two-thirds of the southeast flank is reported to have been 
unusually rich in mica. Pillars in this part of the mine show a mica-rich zone from 6 inches to 2 feet thick 
along the contact between the pegmatite and the granite. The zone contains from 10 to 40 percent of mica in 
books as much as 18 inches in diameter. The zone appears to fade out toward the northeast along the south- 
east flank, and there is no evidence for the existence of such a zone either along the top of the pegmatite dome 
or in the northwest flank. The mica in the dome and northwest flank of the body appears to have been 
rather uniformly distributed throughout the pegmatite. 

Sylva District, North Carolina 








1 5 

o o "^ 

6 S 

u ... c 

c *: ^_ 

o ° £ 













i— i 









32 Mica Deposits of the Franklin- 

The mica is light rum to greenish rum ; its principal defects are warping, small dark-brown to black 
mineral inclusions, green color mottling, cracks, and some ruling. Although the mica is commonly associated 
with biotite, intergrowths of the two minerals are not common. The mica books are hard, split well, and 
are generally free from reeves and "A" structure. It is reported that the mica obtained from around the 
nose was of somewhat better quality than mica from the flanks of the body. For the period November 10, 
1942 to May 4, 1944, the percentage of mine-run mica in pegmatite was 2.8 and the percentage of No. 1 and 
No. 2 sheet and punch mica recovered from the mine-run was 8.6. 


D. M. Larrabee and E. Wm. Heinrich 

The Bowers mine is 3*^ airline miles S.41°W. of Cullowhee, Jackson County. It lies 2,000 feet north- 
west of Presley Creek on a steep east-facing slope, at an altitude of about 3,000 feet. The deposit was 
discovered in 1899 and has been intermittently operated to the present time. In 1929 it was purchased by 
R. U. Garrett of Sylva, who sold it to the Rubin and Hetkin Mica Company of Sylva. This company operated 
the property for 18 months ; it was then sold to Philip Godley of Pittsburg, Pa., who worked it for about 6 
months. The mine was repurchased by Garrett and again sold to the Rubin and Hetkin Mica Company, who 
have continued operations to the present time. 

The workings consist of a narrow open-cut 150 feet long and 15 feet in average width. (See pi. 9.) 
From this cut stopes, drifts, and inclines, all interconnected, extend to the west and southwest. The differ- 
ence in altitude between the highest lip of the cut and the lowest underground workings is 140 feet. 

The country rock, a banded garnetiferous quartz-biotite gneiss, strikes generally northeast and dips from 
80° southeast to 60° northwest. This rock has been injected by a pipe-like body of pegmatite, which strikes 
N.35°W. and dips 80° southwest on the average. The top of the body is well exposed in an irregular drift 
from the top of the open cut, and it probably plunges at a moderate angle to the northwest. 

The pegmatite contains a quartz core associated with minor quantities of white, blocky microcline. This 
core is surrounded by zones of medium-grained plagioclase-quartz rock containing scattered books of musco- 
vite. The accessory minerals, which are commonly found near the contact with the gneiss, are garnet, pyrite, 
and pyrrhotite. Plagioclase associated with the sulfides is stained a deep green. 

Mica occurs in pipe-like bodies in "rolls" along the hanging-wall contact with the gneiss. These bodies 
plunge 45°NW. and probably reflect the general plunge of the pegmatite mass. They are known as "barrels" 
by the miners, and are as much as 15 or 20 feet thick. Four main "barrels" have been mined, but only one 
appears to have persisted throughout the entire vertical extent of the workings. On the 2,936-foot level the 
quartz core pinches out toward the west and is supplanted by a central zone of very coarse-grained quartz and 
plagioclase. Very little mica was found in this part of the deposit. 

The mica is light rum and is cracked and warped. "A" structure, mineral specks, and inclusions are 
generally absent, but some of the books contain intergrowths with biotite and others are tanglesheet. The 
average mica content of the pegmatite is calculated to be about 2 % ; however, a much higher percentage 
may have been present in the richer parts of the pipes. The percentage of sheet and punch mica in the 
mine-run is calculated to be between 3% and 4%. 


W. C. Stoll 

The Cox mine was first opened in 1868 by Judge D. D. Davies and F. S. Orum. The principal opera- 
tions since that time were for six months in 1896, 1916-19 and 1925-27 by W. A. Rodgers, 1929-30 and 1935- 
37 by the Carolina Mining Company, and 1937-39 by the Asheville Mica Company. L. H. Goodman reopened 
the mine during August 1942 but abandoned it in April 1943. 

In the main workings, two parallel east-striking pegmatites, referred to herein as the North and South 
pegmatites, have been mined for mica. (See pi. 10.) The enclosing wall rock is mica gneiss, the foliation of 
which is generally parallel with the pegmatite contacts but locally is transected by them. 

Sylva District, North Carolina 





inclined m annuo* to 

I'.-er levels 

\\, ) , 2980' LEVEL 

2938 LEVEL 



Mopped by D M Lorrabe-.C Wm Henrtch, 
and RA.Swomon. 1*13*44 

Underground remapped by £ Wm Heinncr. 
ond R.WlaiU. 9-12-44 




2922' LEVEL 

20 40 60 00 



Dump (in taction) 
Quorlt- feldspar pegmatite 
Coarse quo rtz-microc lint pegmatite 
Mossive quartz 
Sheet mico 
Biotite gneiss 

Contact, location accurate, shoving dip 

Contoct, location approximate 

Contoet between pegmatite units 

Altitude of (diot'iof. 

Limit of eipoure 

Rim of open cut 


Upper inclins ^ 

2960' level 

2938* level 

2922* level 

Outlines of 
underground workings, 


Map and Sections of the Bowers Mine, Jackson County. 

34 Mica Deposits of the Franklin- 

The North pegmatite has been developed over a strike length of 220 feet and a width of 30 to 60 feet, in 
an open pit and in underground stopes. The upper contact of this body has the form of an anticline, the crest 
of which pitches 10 degrees in a S.68°W. direction. The axes of minor crenulations in the gneiss pitch parallel 
to the main structure. The south limb of the anticline dips 50°-60°S., and the north limb, where observed, 
dips from 40°N. to 70°S. 

The North pegmatite may be divided mineralogically into two principal zones, each of which comprises 
two types of pegmatite. The upper zone, 2 to 8 feet thick, is represented either by a mixture of light-gray 
plagioclase, light-gray microcline, and quartz or, less commonly, by a mixture of quartz and small books of 
muscovite. Shoots rich in book mica lie in the upper zone, but are not coextensive with the zone. In the 
stopes underground the upper zone has been mined but the lower zone left in place. The lower zone, 6 feet or 
more thick, is mostly massive white quartz, but partly a mixture of coarse microcline with subordinate 
quantities of quartz and small scales of greenish muscovite. 

The South pegmatite, 40 feet from the North on the main level, has been mined over a strike length of 
120 feet and a dip distance of 15 to 30 feet. The walls are curved irregularly, and the dip ranges from 35° to 
70°S. The pegmatite body is 7 to 12 feet thick, and consists of light-gray plagioclase, light-gray microcline 
in variable amounts, quartz, and a few muscovite blocks. 

From the main open-cut and stopes, two parallel series of trenches and small surface workings extend 
east-northeast diagonally up the slope. A single series of cuts extends 1,000 feet westward; these cuts ap- 
parently were excavated in the South pegmatite. The North pegmatite plunges beneath the surface within 
the limits of the main workings, and to the west it lies well beneath the range of surface prospecting. 


E. Wm. Heinrich 

The Engle Cope mine is 71/2 airline miles S.23°W. of Dillsboro, Jackson County. It lies 1,200 feet above 
Savannah Creek and U. S. Highway 23, and about half a mile west of the Cowee sawmill. The mine is under 
lease to L. H. Goodman of Biltmore, N. C, who began operations in December 1943. The workings consist of 
four large open-cuts, five short crosscuts with drifts, all now partly caved, and numerous small prospect pits 
and trenches. The operations by L. H. Goodman have been confined to the large, narrow open-cut near the 
center of the mapped area and to an incompleted crosscut 275 feet northeast and 75 feet below this main cut. 
(See fig. 3.) This crosscut was driven for a distance of about 80 feet, but was then abandoned. If the peg- 
matite body persists with depth this crosscut should intersect it 120 feet from the portal. In March 1944 the 
open-cut had attained a maximum depth of 16 feet and was being deepened over a length of 30 feet and a 
width of about 5 feet. 

The country rock, which is a fine-grained, garnetiferous biotite gneiss, is highly fractured, and the atti- 
tude of its foliation varies considerably. Near the contacts with the pegmatite body the foliation is, in general, 
conformable. The pegmatite is a persistent, tabular, sill-like body striking N.5°E. and vertical or dipping very 
steeply to the east. It ranges in thickness from 2 to 8 feet, and has been explored over a strike length of 
about 1,000 feet. 

In general, the pegmatite is poorly differentiated. However, in an old drift 60 feet south of the main cut 
the body contains a 4-foot quartz core flanked by zones of medium-grained quartz-feldspar rock. A well- 
defined zone of coarsely crystalline muscovite occurs along the western contact with the gneiss, both in this 
drift and in the main open-cut. The quartz core is absent from the open-cut, where the main mass of the 
body consists of a uniformly medium- to coarse-grained intergrowth of quartz and plagioclase. Near the 
west-wall mica zone much of the plagioclase is partly replaced by dark-green sericite. Small red garnets 
and small blebs and veinlets of pyrrhotite occur sparingly in the plagioclase. Near the contacts with the peg- 
matite body the gneiss contains thin films of both pyrite and pyrrhotite. 

Mica occurs in a west- wall (generally the hanging- wall) zone. This zone, which is well defined both in 
the main open cut and in the old drift south of the cut, is poorly defined in the workings at the northern end 
of the area. In the cut this zone has a maximum width of 2 feet and books of mica as much as 7 inches in 
diameter were observed in it. At the north end of the cut this zone was estimated to contain between 5 and 
8 percent of book mica. 

Sylva District, North Carolina 



— 2540 




TK ^^ 



A -A' 



Massive quartz 

Sheet mica concentration 

Microcline-plagioclase -quartz pegmatite 

Plagioclase-microcline- quartz pegmatite 

Quartz with small (1/4-1/2") mica flakes 

Ptagioctase with garnet and quartz 

Contact, location approximate 

Contact between pegmatite units 

Strike and dip of foliation 

Strike of vertical foliation 

pitch of axis of small synclinal fold 

Limit of exposure 

Outline of underground workings 

Outline of stope at waist level 



( burr ) 

Rim of open cut 

Scale in feet 
(for map of main workings ond sections) 

40 C 

Mapped by W. C. Stolt and J. J. Norton 
February 1943 

Scale in feet 
Contour interval 20 feet. Datum assumed. 

Map and Sections of the Cox Mine, Jackson County. 


Mica Deposits op the Franklin- 

Dump (in section) 

Quorlz-feldspor pegmotite 

Massive quartz 

Sheet mica 
j 1 Biotite gneiss 
J^"" Contact, locotioo accurate, showing dip 
- — ' Contoct, location approximate 

Contact between pegmatite units 

s<7s Attitude of foliotion 
Limit of exposure 

Outline of underground workings 

j<^ Rim of open cut 
*""""'"" Margin of dump 



Mapped by E.Wm.Heinrich and M.R.KIepper 





Scale in feet 

Fig. 3. — Map and Sections of the Engle Cope Mine, Jackson County. 

The mica is light rum ; some of it has a light-greenish cast. Much is slightly wavy and soft. A high 
proportion contains a light-green mottling, but iron oxide spots are uncommon. Reeves and cracks are 
subordinate and "A" structure occurs chiefly in the larger books. 


D. M. Larrabee 

The Frady mine is 3i/ 2 miles N.85°W. of Cullowhee, Jackson County, near the top of a northward- 
facing ridge. 

The mine is said to have been opened about 60 years ago by C. and E. Bowers, of Webster. M. D. 
Cowan, the present owner, has operated the mine from October 1942 to the present (October 1944). Devel- 
opment consists of a main adit, the Bowers adit, several short adits, stopes, and open cuts, and shafts to a 
depth of 135 feet. These workings form a series 650 feet long trending about N.60°W. 

Sylva District, North Carolina 37 

Three pegmatite bodies are exposed on the property, but nearly all of the mica has been obtained from 
one. This main pegmatite is 4 to 8 feet thick and consists of a central core of quartz flanked by narrow 
margins of plagioclase, quartz, and muscovite. A few red garnets are present near the contacts. Microcline 
is associated with the central quartz masses. The muscovite, which is rum to ruby and slightly stained, is 
associated with the contacts rather than with the quartz masses. The mica zones are richest along the foot- 
wall contact, where the books are also largest. This zone is richest over a 6-inch width which occasionally 
widens to 12 inches. The hanging- wall mica zone is of equal width but is leaner ; the mica therein is smaller 
but of darker color and better quality. 

The country rock is biotite gneiss with occasional layers of hornblende gneiss. The foliation strikes 
northwest and dips steeply northeast. Although the pegmatites generally parallel the foliation, trending 
northwest and dipping steeply northeast, they are locally discordant. All rocks have been subjected to much 
faulting of apparently small displacement. As a result many of the mica books are badly folded, bent, ruled, 
and warped. 


D. M. Larrabee 

The Iotla-Bradley mine (also known as the Iotla or Iotla Bridge mine) is 4 airline miles N. 10°W. of 
Franklin, Macon County. It lies at an altitude of about 2,000 feet on the west bank of the Little Tennessee 
River at the mouth of Iotla Creek. The mine was first operated in 1905 by Francis A. Gudger, who later 
leased it to the Southern Mica Company. This company mined it for both kaolin and mica for about 10 
years. In 1935 Charles Bradley of Franklin leased the property and operated it as a scrap and sheet mine 
until 1940, when the Bradley Mining Company was formed. Bradley relinquished his interest in this com- 
pany in 1944 and the present officers are Messrs. Preston, Lee, and Zieseniss of New York City. 

The workings consist of a large open-cut which is 800 feet long, averages 200 feet in width, and has a 
maximum depth of about 160 feet. (See fig. 4.) Older workings consisted of several shafts and adits, many 
of which have been completely destroyed or rendered inaccessible by the open-cut operation. 

A large irregular body of pegmatite has been explored over a length of 800 feet and has a maximum ex- 
posed width of 200 feet. It trends N. to N.30°E. and is vertical, cutting across the foliation of biotite gneiss. 
The walls are extremely irregular, and large septa and inclusions of wall rock are common near the margins 
of the mass. 

The pegmatite body is poorly zoned and consists of a medium-grained aggregate of kaolinized feldspar, 
muscovite, quartz, and a little biotite. Several small auartz pods occur near the south end of the open-cut and 
a large quartz rib as much as 120 feet long and 15 feet thick lies near the western contact at the north end 
of the main open-cut. 

Mica of scrap grade is uniformly distributed throughout the mass of pegmatite, but sheet mica is con- 
fined to zones surrounding the large quartz rib. The scrap mica occurs in scattered books and flakes generally 
less than 2 inches in diameter, and is of deep-rum color. The mica-rich zones along the quartz rib contain 
books as much as 2 feet in diameter. This mica is of deep-rum color, is ruled, and some of it contains "A" 
structure.. In general, however, books from this zone are hard and flat and of excellent quality. 

The deposit has been operated chiefly for kaolin and scrap mica with by-product sheet mica. The quarry 
has been developed by benching with gasoline shovels. The ore is loaded by shovels into trucks and hauled 
to a small jaw crusher at the bottom of the main pit, where it is broken and washed into a bucket conveyor 
that carries it to the rim of the open-cut. From there the ore goes by flume to the mill, where the stream is 
split to feed two similar units. The material passes through two sets of rolls and trommel screens before 
reaching the drying bin for draining. It is then put through a wood-fired rotary dryer, and thence passes 
to another set of rolls and a trommel screen. Mica to be sold as jigged scrap goes directly to storage bins 
for bagging; that which is to be pulverized before sale passes through a Raymond mill. 

The production of scrap mica is reported to average 3,000 tons per year. Mica constitutes about 10 
percent of the rock moved. Sheet mica production was considerably curtailed after June 1944 because the 
sheet mica zones were partly covered by large slides of material from the walls of the cut. Selected mine- 
run mica from the mica-rich zones contains about 8 percent of sheet and punch mica. 


Mica Deposits of the Franklin- 

: 3j Biotite gneiss 

j Contoct, locotion occurole, showing dip 
/ Contoct, location opproximote 

Contact between pegmatite units 
Attitude of foliotion 
Limit of exposure 
Rim of open cut 

Outline of* underground workings 
Margin of dump 
50 100 


Fig. 4. — Map of the Iotla-Bradley Mine, Macon County. 


E. Wm. Heinrich 

The Riser mine is 4 airline miles S.87°W. of Franklin, Macon County, at an altitude of 2,300 feet on the 
west side of a small tributary of Mill Creek. The mine is owned by J. Burn Riser of Route 1, Franklin, and 
only prospecting was done before 1942. George Scott of Franklin operated the mine from November 19, 
1942 to May 8, 1944, at which time A. W. Reid of Franklin secured the lease and continued operations until 
late November 1944. 

The workings (pi. 11) consist of an open-cut 145 feet long, 65 feet in maximum width, and 35 feet in 
maximum depth, and a shallow bulldozer trench to the south. Both the country rock and pegmatite are 
decomposed, and large slides from the walls of the cut are common. 

Sylva District, North Carolina 





Mopped by EWm Heinnch, LC Proy, MR Klepper, 
3-1-44 ond 5-2-44. Remopped by R.W Lemke 
ond EWm Heinnch 11-16-44 


Dump (in section) 

Quortz-feldspor pegmotile 

Sheet mica 

Gneiss with injected granitic moterial 

Biotite gneiss 

Contact, location accurate, showing dip 

Contact, location approximate 

Attitude of foliation 

Limit of exposure 

Rim of open cut or trench 



Map and Sections of the Riser Mine, Macon County. 

The open-cut exposes a single pegmatite body that strikes N.45°E. and appears to be vertical. The 
country rock is a fine-grained biotite gneiss, whose vertical foliation strikes a few degrees north of west. The 
pegmatite cuts across the foliation, and the contacts between the two rocks are irregular in detail. The 
pegmatite mass has a maximum thickness of 25 feet, and has been exposed over a distance of 250 feet. At 
the north end of the cut it pinches out in a hook-shaped nose and is supplanted along its trend by a zone of 
gneiss impregnated with many small pods and stringers of pegmatitic material. 

The pegmatite is a medium- to coarse-grained intergrowth of quartz, feldspar, and muscovite. Biotite 
is rare. Muscovite occurs in zones along both walls. The quantity of mica is unusually large, but the general 

40 Mica Deposits of the Franklin- 

quality is poor. Clusters of books as much as 4 by 6 feet in area have been mined, and books as much as 1 
foot in diameter are common. In general the mica is soft, badly cracked, and stained with a light-green to 
light-brown, fuzzy mottling. Specks of iron oxide are rare, however. The mica occurs in two colors — green 
and light rum. The latter is uncommon and probably constitutes only a few percent of the total mine-run 
mica. In general the light-rum mica is very flat and of much better quality than the green mica. 


J. M. Parker III and W. C. Stoll 

The Lyle Knob mines lie on the southwest and west slopes of Lyle Knob, 4.9 miles N.12°E. of Franklin, 
Macon County, at altitudes between 2,900 and 3,300 feet. (See pi. 12.) They include 8 large open-cuts 40 to 
275 feet long, 9 tunnels 50 to 340 feet long, at least 14 smaller tunnels, several shafts, and many prospect 
pits. The majority of these are grouped at the south end of the area, and constitute the Lyle Knob mine. 
Two tunnels and an open-cut 1,200 feet north are called the Buttermilk mine. The two long narrow cuts on 
the hillside between these two mines are the Siphon and Borrows cuts. 

The first mining on Lyle Knob was done by A. S. Bryson about 1880. He sank the Bryson shaft on the 
ridge and opened the Bowers Cut, with highly successful results. The mine also was operated from 1899 to 
1901, for several years about 1910, and during the first World War. About 1935, the big south cut was 
worked for scrap mica by Duval and Shields. The National Mica Company operated the mine from July to 
December 1942, and intermittently during the early part of 1943. 

The area is underlain by gray biotite gneiss, generally distinctly banded. It consists of biotite, musco- 
vite, feldspar, quartz, and local pink garnets. The general trend of the foliation of this rock is northeast to 
east, with steep dips to the northwest and north. The layers are highly contorted. At least 10 pegmatite 
dikes occur in the area. They trend east to northeast, dip northward at various angles, and are approxi- 
mately conformable with the foliation, although commonly they cut across it in detail. They range in thick- 
ness from one to 40 feet. Abrupt changes in strike, dip, and thickness are common. 

The lower workings on the west slope of the ridge include four large open-cuts and at least three adits. 
The pits are slumped and the adits flooded so that little could be learned about the western and lower parts 
of the deposit. In the big south cut the pegmatite, about 40 feet thick, consists mainly of kaolinized feldspar 
with small scattered quartz masses. In the Bowers and other cuts just to the north is a pegmatite that prob- 
ably is a branch of the main dike. It is about 25 feet thick in the Bowers cut, but thins to a mere stringer 
in the cut to the northeast. Here it plunges 35 degrees S.55°W., seems to occupy the crest of an anticline in 
contorted mica gneiss, and has irregular apophyses which extend into cracks and foliation partings. The 
pegmatite has many small inclusions of gneiss and much quartz in irregular masses. Mica in books as much 
as three inches in diameter is fairly plentiful. Curved, biotite-coated shear fractures in quartz lie parallel 
with the contact in one part of the pegmatite. 

The main pegmatite at the east end of the workings is reached by tunnels 1, 4, and 5. It was mined at 
its upper end from the old Bryson shaft, and underground by means of one large stope with subsidiary stopes 
and crosscuts. These workings expose the pegmatite intermittently over a strike length of nearly 300 feet 
and a dip distance of about 100 feet. The pegmatite is an elongate lenticular body, shaped like a flattened 
cigar or bean pod, with an irregularly elliptical cross section. In general the body trends east and dips 
steeply northward, and plunges to the west at an angle of about 25 degrees, though it curves and bends 
abruptly at several places. The upper end is exposed in the Bryson shaft and the top edge is also exposed in 
the big south cut. The shorter axis of the elliptical cross section ranges from 15 to 30 feet, and the longer is 
about four times as great. 

The pegmatite is composed of plagioclase, microcline, quartz, muscovite, biotite, garnet, and pyrite. 
The plagioclase is white and is generally altered to soft kaolin; even at the lower levels of the mine the 
plagioclase has a chalky appearance. Light-gray microcline is more abundant than plagioclase, and is partly 
intermixed with quartz. The quartz is light gray and glassy, or white and sugary. Pink garnets, in crystals 
as much as half an inch in diameter, and biotite are relatively scarce. The muscovite is clear ruby. 

The pegmatite is irregularly zoned. Mica-bearing zones 1 to 5 feet thick generally occur along both the 
f ootwall and the hanging wall, where block mica is irregularly scattered in a matrix of microcline and subor- 

Sylva District, North Carolina 



3119 3B6 


O •? ia ^>! 

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20 40 60 

Scale In feet 

Massive quartz 
Pegmatite with sheet mica 
Pegmatite with scrap mica 

I ° & a \ Microcline pegmatite 


I* *-*-*] Plagloclase pegmatite 

Pegmatite, undifferentiated 

[t^l^H M'ca gneiss 

S*7o Contact, showing dip 

„--- - Contact, approximate 

■- — Contact between pegmatite -units 

--*-». Strike and dip of foliation 

— ■*"" Strike of vertical foliation 

-- * Trend of pegmatite body 

(il'lS*- Outline of underground workings, showing altitude of floor 

— -fl Caved end of adit 

H Rim of open cut 

^ / Dump 

Datum is mean sea level 
Mapped by W.CStotl and J. M. Parker III April-May 1943 


/^ Pr 

•p 3200 

/ // // 

/ .<*' ^~ '■'' 

/ >? -'7 -^ 

./ ,o'' c --' „ — ?' 


^i."«»'«"''^--'''>* , ' , 

^„--~ - 


.? — '- 

/ '„---'' 







Map and Sections of the Lyle Knob Mine, Macon County. 

dinate plagioclase and quartz. At the No. 4 level the south-wall mica zone is reported to be the more pro- 
ductive, whereas at the No. 1 level and below it commercial quantities were obtained only from the north 
side. Pegmatite that consists chiefly of microcline, with minor plagioclase and quartz lies next to the mica- 
bearing zone, and in the upper part of the mine it is the innermost zone of the dike. Where mica-bearing 
pegmatite is absent, the microcline pegmatite may extend to the walls. A core of massive quartz occurs in 
the lowest (west) part of the No. 1 stope and in the No. 5 tunnel but is absent from higher levels. It is 
flanked by microcline zones without any sheet mica. 

The other pegmatites in the Lyle Knob area are composed dominantly of plagioclase with minor quartz 
in small masses and relatively little commercial mica. This type of plagioclase pegmatite is rarely encoun- 
tered in the main Lyle Knob mine. 

42 Mica Deposits of the Franklin- 


J. M. Parker III and W. C. Stoll 

The Moody mine, northwest of Franklin, Macon County, was an exceptionally productive mine during 
part of its history. (See pi. 13.) The forked drift on the south side of the ridge was driven about 1900, 
but very little mica was obtained. About 1914, Ray and Fouts worked in the weathered part of the main 
pegmatite to a depth of about 50 feet below the outcrop. Many of these upper workings are caved and no 
longer accessible. Frank Moody operated the mine successfully for three years about 1917, driving at least 
two short adits, lower and farther west than Ray and Fouts. Later he drove the lowest adit, 250 feet long, 
and opened most of the workings at this and lower levels. The mine was then operated without great success 
by a Philadelphia company in 1920 and 1921, and was idle from 1922 until September 1942. W. E. Grind- 
staff then reopened it for the Asheville Mica Company, and the operation continued intermittently until late 
in 1944. 

The wall rock is a relatively fine-grained gneiss consisting of quartz, feldspar (mainly plagioclase) , bio- 
tite, muscovite, and small pink garnets. The gneiss is layered, some bands being schistose, others fine-grained 
and granitoid. One hundred feet or more from the pegmatite, the gneiss strikes about N.15°E. and dips 50 to 
60 degrees northwest, but near it the foliation has been twisted in many directions. 

The pegmatite body trends east across the foliation of the country rock. Its strike changes markedly in 
the middle of the workings, forming a crude, elongate "S" in plan. As traced from the east end, the dike 
bends from slightly north of west to about S.60°W. in the center, and back to west-northwest at the west end. 
The average dip from the surface to the lowest workings is 74°. 

The pegmatite contains a core of quartz that is nearly ten feet thick at the center of the mine. Between 
this mass and the walls on either side are feldspathic zones each 4 to 6 feet thick. The central quartz body 
pinches out to the east in the lower levels so that the hanging-wall and footwall feldspathic zones merge, with 
a total thickness here of 5 feet or less. The quartz continues to the west as far as the mine has been de- 
veloped. The quartz mass is cut by many closely spaced shears, especially near its footwall margin, that are 
approximately parallel to the sides of the quartz mass. They are coated with biotite, as much as 0.2 inches 
thick, and where the shears are closely spaced, the rock has a schistose appearance. 

The feldspathic pegmatite consists mainly of bluish-gray plagioclase and quartz, with muscovite, and 
a little biotite and garnet. No microcline was observed. Along the walls in many places is a 6- to 8-inch 
border zone of finer plagioclase and quartz, studded with small mica books one-quarter of an inch to one inch 
in diameter. Within the feldspathic wall zones mica is concentrated in certain shoots, the richest of which 
are in contact with the central quartz zone. Where the quartz core is absent, as at the east end of the mine 
on the lower levels, the mica is cracked and wavy. 

The workings as a whole plunge downward S.55°W. from the surface at an angle of 60° — the probable 
pitch of the quartz core. It seems likely that the quartz core and the mica shoots are related to the changes 
in strike of the dike as seen in the accessible underground workings, and possibly also to a decrease in dip of 
the body at about the adit level. 


E. Wm. Heinrich 

The Poll Miller mine is on the north side of Tremont Ridge, 8 airline miles N.80°W. of Franklin, Macon 
County. It lies on the east side of Miller Hollow at an altitude of 2,800 feet and is about li/ 2 miles northeast 
of Locust Gap. It is reported that the mine was opened in 1900 and that much of the early work was done 
by Charles Bowers of Franklin, who later sold the mine to a Mr. Clarke. The mine was idle for about 25 
years except for minor near-surface operations and reworking of the dumps. Early in 1943, Messrs. Lowell 
Jamison, Fred Arnold, G. A. Jones, Richard Jones, W. Rogers, Frank Moody, Mark Dowdle, and Henry Cabe 
of Franklin, purchased the property. They began operations in July of that year. 

The workings (pis. 14 and 15) consist of a stope 120 feet deep, two adits, and an inclined shaft along 
the northeastern edge of the stope. The stope, which has been partly backfilled, opens to the surface. It 
was worked chiefly through Adit B, which is a 150-foot crosscut that is blocked by muck a few feet from its 
junction with the stope. *Adit A, at the southern end of the area, is a 75-foot drift with overhand backfilled 
stopes that probably extend to the surface. 

Sylva District, North Carolina 

















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Mica Deposits of the Franklin- 





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46 Mica Deposits of the Franklin- 

The country rock is a banded biotite gneiss, whose foliation strikes from W. to N.65°W. and dips steeply- 
north to vertical. This rock has been cut by a body of pegmatite which strikes N.25°E. and dips 55° south- 
east. Along the hanging wall of the pegmatite the foliation of the gneiss swings sharply toward the north- 
west. It seems likely that the body was emplaced along a fault. The change in trend of the gneissic foliation 
along the contact is evidently a result of movement of the hanging wall toward the southwest. 

The pegmatite body, which has a maximum thickness of 8 feet, contains a central 3-foot quartz core. 
Both the dike and the core plunge northeast, the dike 24° and the core about 40°. Toward the southwest, 
in Adit A, the quartz core is supplanted by a thick central rib of coarse blocky microcline. The core is flanked 
by pegmatite rich in feldspar (chiefly plagioclase), which contains much coarsely crystalline muscovite. Ad- 
jacent to the quartz core the plagioclase has been stained a bright green and contains veinlets of pyrrhotite 
as much as 3 inches long and V2 inch thick. Above the quartz mass, — that is, to a depth of about 50 feet in 
the shaft — the pegmatite is a feldspar-rich rock containing abundant small flakes of muscovite, small pods 
of "burr rock", and scattered lenticular inclusions of gneiss. Biotite and garnet are accessory minerals. 

The microline core exposed in Adit A grades to the southwest into medium-grained feldspar-quartz peg- 
matite. The microcline blocks, some of which are as much as 2 feet thick, are transected by veinlets of quartz 
and fine-grained muscovite. Concentrations of coarsely crystalline muscovite lie along both sides of the core. 

Books of mica occur in the zones that flank the core of the pegmatite. The mica that occurs in the un- 
zoned parts of the pegmatite body is almost entirely of scrap grade. The books occur in clusters concen- 
trated around the margins of the core. Although most of the mining has been done in the quartz-core part 
of the pegmatite, the mica zones also occur along the microcline core. The mica is light rum, and is generally 
hard and flat. The chief defects are reeves, scattered black mineral inclusions, and a green mottling. "A" 
structure is absent, and flattened inclusions of quartz are rare. Much of the mica is of very good quality. 

Grade of Poll Miller Pegmatite 
(Based on mining between August 26, 1943 and May 4, 1944) 

Total pegmatite mined 300 tons 

Total mica mined* 8,000 pounds 

Percent mica in pegmatite* 1.3% 

Mine-run mica recovered 7,000 pounds 

Sheet and punch mica produced 683.60 pounds 

Percent of sheet and punch in mine-run ♦ 

mica recovered 9.8 % 

*Based on the estimate of 1,000 pounds lost as small broken flakes and larger books in unbroken blocks of 


W. C. Stoll and J. M. Parker III 

Rocky Face Knob, on the line between Macon and Jackson Counties, consists mainly of mica-garnet 
gneiss, with small amounts of biotite-garnet schist and kyanite gneiss. The foliation strikes generally north- 
west and dips north or northeast at steep to moderate angles, but in many places it is contorted irregularly. 
Many pegmatites are exposed on the steep mountainside ; they trend N.N.W. and dip steeply. The positions 
of the seven principal openings in pegmatite are shown on the accompanying map of Rocky Face Knob (fig. 
5) . The workings are all relatively small with the exception of the Rocky Face mine, which has been worked 
intermittently for many years by numerous operators. From 1937 to 1941, it was operated by the Asheville 
Mica Company, and later by D. E. Worley. W. N. Grimm was the operator in March 1943, when the mine 
and nearby pegmatites were mapped. 

The main pegmatite, 6 to 18 feet thick, is enclosed in biotite-garnet gneiss, and partly cuts across the 
foliation. Smaller pegmatite bodies, 1 to 7 feet thick, occur in the footwall and hanging wall, and are probably 
connected with the main pegmatite. The main pegmatite body, mined in stopes No. 1 and No. 2, has yielded 
most of the sheet mica. Stope No. 3, forming the north part of the mine, was excavated in a closely related 
pegmatite that probably joins the body mined in stopes 1 and 2. The mining of stope No. 3 was done mostly 
by the Asheville Mica Company. 

Sylva District, North Carolina 


from wall of open cut} 


Pegmatite with much small mica 

Plagioclase pegmatite 

Quartzose pegmatite 
[isLM Garnet-mica gneiss 

-~!s*' Contact, showing dip 

^2-* — Strike and dip of gneiss foliation 

^*-v Strike of vertical foliation 
C ^Z~ Outline of underground workings 

If' Caved workings 
D Shaft 

^* Rim of open cut 

S"< Dump 

Mapped by J. M. Parker III and W.C. Stoll 

Scale in feet 

Contour interval 40 feet 

Datum assumed 

Fig. 5. — Map and Sections of the Rocky Face Mine, Macon County. 

The part of the main pegmatite body, exposed in stopes No. 1 and No. 2 from which most of the sheet 
mica has come, has a strike length of about 100 feet and a maximum thickness of 18 feet. It consists of an 
irregular core 3 to 6 feet thick of white sugary quartz, separated from both walls by feldspathic zones in which 
the commercial mica books occurred. At the north end of this part of the mine, the quartz core pinches out and 
the thickness of the pegmatite body diminishes to 6 feet. At the south end, in stope No. 1, the pegmatite 
terminates bluntly, but it is succeeded to the south by other, apparently unconnected pegmatite bodies. 

The feldspathic parts are composed principally of white plagioclase with a little microcline, minor 
amounts of quartz, muscovite, and small garnets. The footwall feldspathic zone is 7 to 11 feet thick; the 
hanging-wall feldspathic zone is mostly about 3 feet thick, but rarely it is absent and the massive quartz lies 
next to the hanging wall. 

Mica from the Rocky Face mine is clear ruby of very good quality. Some of the sheets are slightly wavy, 
but staining and other imperfections are not conspicuous. Sheets of relatively large size have been obtained 
from some mica books mined from the pegmatite of the Rocky Face mine. 


E. Wm. Heinrich 

The Sheep Mountain mine, 7 airline miles S.25°E. of Sylva, Jackson County, lies on the north side of Moses 
Creek, about 200 feet above the Moses Creek Road. The mine is owned by the Blackwood Lumber Company 
of East Laport, N. C. It was worked intensively from 1915 to 1918 by Oscar Lovedahl of East Laport. In 
March 1944 it was leased to J. W. Swayangim and Oscar Lovedahl, who planned to reopen the mine, but this 
plan was later abandoned. 

48 Mica Deposits op the Franklin- 

The main group of workings (pi. 16) consists of an open-cut 100 feet long, as much as 45 feet wide, and 
75 feet deep at the face. An adit extends northeast for 65 feet from the northeastern corner of the cut. 
From the end of the adit a crosscut is inclined upward and to the east for 20 feet. A large, irregular stope 
65 feet long and as much as 25 feet high extends toward the northeast from the northwestern corner of the 
cut. Seventy-five feet south of the main open-cut is a caved adit. As its dump contains no pegmatitic debris, 
the adit probably did not reach any pegmatite. About 200 feet southwest of the open-cut, and beyond the 
mapped area, are two shallow, irregular cuts and several caved adits. 

The country rock is a fine-grained quartz-biotite gneiss, whose foliation strikes northeast and dips steeply 
northwest to vertical. Near the main pegmatite body many stringers of quartz are present in the foliation 
planes of the gneiss. The pegmatite body is Y-shaped in cross section. The two arms of the Y converge 
near the bottom of the face of the open-cut to form a trough, the axis of which plunges to the southwest at a 
low angle. The two arms of the Y are exposed on the upper parts of the face and crop out northeast of the 
cut. They strike northeast and are vertical. The pegmatite has been explored over a length of 170 feet and a 
vertical distance of 120 feet. The stem of the Y has a maximum thickness of 20 feet, and the arms range in 
thickness from 3 to 5 feet. 

The pegmatite consists chiefly of plagioclase with varying amounts of biotite, quartz, and muscovite. In 
general biotite is the most abundant mineral, forming as much as 60 % of the rock in some places. It occurs 
in warped books as much as 8 inches in diameter and in dense aggregates of small flakes. Some of the plagio- 
clase occurs as euhedral crystals "wrapped" in sheets of biotite that are curved to follow the outlines of each 
crystal. Thin, discontinuous quartz ribs were noted in the south end of the stope from the open-cut. 

The most important mica concentration appears to have been along the west wall of the stem of the Y, 
and was mined in the open-cut and in the adit from the cut. A subordinate mica zone is exposed in the cross- 
cut from the adit 10 feet west of the eastern contact cf the stem of the Y. In addition, books of mica occur in 
both arms of the Y, but they are only locally abundant. The mica is dark brown and occurs in books as much 
as 6 inches in diameter. The average diameter, however, is less than 3 inches. The crystals are commonly 
euhedral and are unusually hard. Very little of the mica is warped, but reeves are common. Nearly all of the 
books contain a central core of light-spotted mica. Although much of the muscovite is closely associated with 
abundant biotite, intergrowths of muscovite and biotite are uncommon. 


J. C. Olson 

The Shepherd (Boyd) Knob pegmatite trends north across the south side and top of a low ridge which 
rises about 500 feet above the level of Cowee Creek, a quarter-mile south of the mine, (see pi. 17) 6V2 airline 
miles north of Franklin, Macon County. During the last 20 years it has been one of the largest sources of 
scrap and sheet mica in the district. Both kaolin and mica were mined as early as 70 years ago from tunnels 
and pits in soft decomposed pegmatite. Adits, begun near the crest of the ridge, were driven progressively 
lower on both the south and north slopes of the ridge. The lowest adits north of the ridge, the Bob and "New" 
adits, were driven about 1917-18 ; the Bob adit is reported to have been driven through the mountain to the 
main open-cut. Most of the adits on the north side of the ridge are open and accessible to their intersections 
with the pegmatite, where they are caved. It is reported that much stoping was done eastward from the 
ends of these adits along the pegmatite, but very little westward except for a reported 60-foot drift west- 
ward from the Bob adit. 

Several years after World War I, J. E. Rice installed a plant for the recovery of scrap mica from decom- 
posed pegmatite by washing and screening. This hydraulic mining obliterated many of the older "ground- 
hog" tunnels, and created a large (East) open-cut 350 feet long and as much as 175 feet wide and 75 feet deep, 
and a smaller (West) open-cut 250 feet long, 50 feet wide, and 25 feet deep. Subsequently, much scrap and 
some sheet mica have been mined, mostly by J. E. Rickman and by the Asheville Mica Company. Late in 
1941, Newell Hooper drove the lowest (Hooper) adit on the south side of the ridge, and mined sheet mica from 
it until the spring of 1944. 

The pegmatite is enclosed in gray mica gneiss, composed dominantly of quartz and feldspar, with gar- 
nets and flakes of biotite and muscovite so small that weathered rock shows only very faint foliation. The 
gneiss is deeply weathered to a yellowish or purplish- brown color, and is cut by joints and small faults. Some 
of the joints contain pegmatite; others cut both country rock and pegmatite and contain quartz; however, 

Sylva District, North Carolina 






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50 Mica Deposits of the Franklin- 

most of the joints contain no filling and appear to be post-pegmatite. Post-pegmatite faults have resulted in a 
pronounced ruling of many of the mica blocks. 

Mica flakes in the wall rock near the pegmatite body have been greatly enlarged by solutions from the 
pegmatite, and enclose small garnets. Some of the flakes are as much as 1^ inches across. 

The irregular pegmatite body, at least 150 feet thick, consists of quartz, microline, plagioclase, mus- 
covite, and biotite. The feldspar is altered to kaolin near the surface, and is semikaolinized in underground 
workings 140 feet vertically below the top of the ridge. 

On the geologic map (pi. 17) three types of pegmatite are distinguished: (1) Massive quartz, in a body 
at least 20 feet thick, forms a very prominent core of the pegmatite. "Burr rock" occurs in places near the 
margins of the quartz core. (2) The pegmatite separating the quartz core from the hanging wall is com- 
posed of quartz, feldspar (dominantly plagioclase) , muscovite, and a little biotite. In this zone, about 10 feet 
thick, the main mica-bearing streak occurs. This mica zone is exceptionally rich in muscovite, although the 
average size of sheets obtainable is fairly small because the blocks are ruled, commonly in two directions, to 
yield diamond-shaped sheets. Very little mica larger than 3x5 inches has been produced. Biotite is 
relatively scarce in this zone and occurs as small strips. (3) Most of the pegmatite body is kaolinized feldspar, 
which occurs either in large, nearly pure masses, or in many masses 11/2 feet or less in diameter and separated 
by finer-grained material. Some of the kaolin masses have a "rounded" outline. The finer-grained interstitial 
material is of three principal types that are intergradational : (a) mostly quartz ; (b) a mixture of quartz 
and small mica, in places biotite, with occasional fine-grained feldspar ; or (c) material relatively rich in small 
muscovite and biotite flakes and resembling the coarse mica schist of altered wall rocks. Type c is more f elds- 
pathic than the others. 

The sheet-mica zone, about 10 feet thick, occurs directly above the main quartz mass, is itself more 
quartzose than the remainder of the pegmatite, and appears to be richest above the thickest part of the quartz 
body. As the mica zone is followed away from this richest portion — for example from the heading south- 
ward toward the portal of the Newell Hooper adit — the quartz and muscovite content diminishes and that of 
feldspar and biotite increases ; correspondingly the main quartz mass becomes thinner. It also becomes thin- 
ner down dip, and the "keel", or point where the quartz disappears down dip, evidently pitches northward at 
an angle of 15 or 20 degrees. 

The thickest part of the quartz body coincides with an upward bulge or "nose" in the hanging wall of the 
pegmatite, which plunges northward from a point at about the 2380-foot level in the northeast corner of the 
open-cut to the north end of the Hooper adit at the 2300-foot level. The upward bulge or nose is indicated by 
the attitude of contacts on both sides of the Hooper adit. The pegmatite is probably richest in mica within 
200 feet of this nose, along either flank. The mica mined recently from the Hooper adit has come from the 
crest and the flank extending southward from the crest. 

The mica is of ruby color, but roughly two-thirds of it has a cloudy stain which, although not black, 
renders it unfit for certain high-quality uses. The clear mica, where perfectly flat, is of excellent quality. 


J. C. Olson 

At the Stillwell mine, 31/2 airline miles south of Sylva, Jackson County, a north-trending pegmatite body 
has been developed by two main shafts, three principal adits from the north, and several smaller adits, pits, 
and trenches. (See pi. 18.) The lowest adit is report 3d to have been started by the Bowers brothers about 
1875, after some mining had already been done near the outcrop of the pegmatite. Work in this adit was in- 
termittent, and it was not until 1885 that John Frady drove the adit through to the mica-bearing pegmatite. 
The early mining from this adit is said to have been confined to the softer kaolinized pegmatite, and for that 
reason its bottom profile rises toward the south. This adit is now in accessible, but apparently intersected 
the pegmatite at a distance of about 210 feet from the portal. 

The Intermediate Adit is reported to have been driven by a Mr. Rogers about the time of the first World 
War. This adit is inaccessible, but extends 175 feet to the Old Shaft, a circular shaft reported to be 18 feet 
in diameter and about 100 feet deep, which it intersects at a point about 40 feet above the bottom. This 
shaft was sunk in 1915-16 by A. R. Stillwell. 

Sylva District, North Carolina 




[ i 






s 5 




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A < 





«^N < 


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V i 









r s. : 





52 Mica Deposits of the Franklin- 

In December 1943, Chester C. Harris of Sylva reopened the mine. The shaft now in use, referred to 
herein as the New Shaft, was sunk, probably on the site of an old shallower shaft, to a depth of 122.5 feet, 
including a 6-foot sump. The first 90 feet of this shaft was in old workings, and the drift northward from the 
bottom also struck the base of the Old Shaft. The Old and New Shafts are 40 feet apart, and the block of peg- 
matite between them is believed to be mostly mined out. The pegmatite has also been mined out north of the 
Old Shaft for a distance of about 40 feet, and perhaps for a shorter distance south of the New Shaft. 

Three parallel north-trending pegmatites have been mined in the area mapped, and another lies 200 feet 
west of the New Shaft. The easternmost is 1 to 2 feet thick ; 35 feet west of it is a pegmatite body 1 to 3 feet 
thick; and 110 feet farther west is the main pegmatite of the Stillwell mine, 1 to 6 feet thick. Another peg- 
matite body has been mined 200 feet farther west. Exposures are present only where excavations have been 
made, but the area between the pegmatite bodies appears to be underlain entirely by mica gneiss. Local 
light-colored layers in the gneiss are thought to represent selective pegmatitization of the country rock. Sev- 
eral quartz lenses about an inch thick occur in the gneiss within 3 feet of the main pegmatite of the Stillwell 
mine at the bottom of the New Shaft. 

In general the foliation of the gneiss strikes slightly east of north and is nearly vertical. The pegmatite 
bodies cut across the foliation at small angles, with trends averaging due north, but at a few places they are 

Two prominent bends, in which the strike changes as much as 35° within a few feet, occur in both the peg- 
matite at the Stillwell mine and the two dikes that are parallel to it on the east. The axes, or lines connecting 
the similar bends in the three pegmatites, have been drawn on the map. The line joining the northern bends, 
passing just north of the New Shaft, trends nearly due east. The line joining the southern bends, near the 
south edge of the map, trends about N.75°W. 

The two parallel pegmatite bodies prospected east of the main workings are thin, feldspathic, and for the 
most part rather homogeneous. The grains are about three-eights of an inch in average diameter. Muscovite 
is present in small books, commonly bent and ruled. Inasmuch as the two eastern pegmatites appear to con- 
tain little mica, the rest of this report is concerned with the main pegmatite of the Stillwell mine. 

This pegmatite vein is essentially vertical. Although dips are as low as 70° to east or west, the vertical 
New Shaft was in pegmatite (or old workings) for its entire depth. The vein is one to six feet thick and is 
composed of quartz, potash and soda feldspars, and muscovite. Its central part, where exposed at the bottom 
of the New Shaft, is massive quartz containing very little feldspar and a few small muscovite flakes oriented 
parallel to one another. The planar structure suggested by the oriented mica flakes is vertical and strikes 
slightly east of north, not quite parallel with the pegmatite body. Toward the north (base of Old Shaft) 
the central zone grades into a quartz-feldspar rock. Toward the heading south of the New Shaft, the central 
zone becomes micaceous, forming "burr rock." 

Between the central zone described above and the walls, the pegmatite is feldspathic. Large mica blocks 
occur near the walls, and tend to be oriented with their cleavages perpendicular to the contacts. One area 
measuring 2 by 6 feet in the south heading was estimated to contain 20 percent muscovite. This was along 
the west wall of the pegmatite ; the feldspathic pegmatite near the east wall contained very little muscovite. 
Near the base of the Old Shaft, however, abundant mica was observed near both walls of the 5-foot pegmatite, 
and it is likely that in the rich parts of the pegmatite both wall zones contain abundant mica. 

The richest part of the pegmatite is reported to extend about 40 feet each way along the strike from the 
Old Shaft, and probably plunges nearly vertically. The pegmatite bends from a northerly strike to N.35°W. 
at the base of the shaft, and this bend may in part be the cause of the local greater thickness. The pegmatite 
appears to thin southward from the New Shaft. In the accessible shallow drifts, it is only 2 to 2.5 feet thick, 
and consists of kaolinized feldspar, quartz, and small muscovite. No well-defined mica zone is present. Irreg- 
ular masses of "burr rock", about 6 feet long and 1 foot wide, are exposed in this drift. Slicken-sided sur- 
faces along the walls of the drifts indicate post-pegmatite faulting. 

The muscovite is light brownish ruby in color and of relatively large size. The sheets are clear, but wavy, 
ruled, or bent blocks are not uncommon. A little "A" mica is reported to have been found near the north end of 
the mica shoot, but only in minor quantities. 

Sylva District, North Carolina 



Map and Sections of the Stillwell Mine, Jackson County. 


E. Wm. Heinrich 

The Tilley mine is 10.3 airline miles N.55°E. of Franklin, Macon County. It lies near the top of the steep 
ridge between Panther and Sheep Knobs. It was mapped by D. M. Larrabee and E. Wm. Heinrich on January 
17, 1944. On September 25, 1944 the underground workings were remapped by R. W. Lemke and E. Wm. Hein- 
rich. The mine, which is owned by the Rubin and Hetkin Mica Company, was discovered in 1935 by R. F. 
Tilley, who worked it for three months. Operations by the Rubin and Hetkin Mica Company have continued 
intermittently to the end of 1944. 

The workings consist of five small open-cuts, one of which leads to a large down-dip stope which has a 
maximum length of nearly 200 feet. The width of the stope at the face is 75 feet. (See fig. 6) 


Mica Deposits of the Franklin- 


— 4060 

x LINE A -A' 

— 4040 


/ ) 

— 4000 


— 3980 

— 3960 ^ 






< V A^^ 










Quartz-plogiocldsa pegmatite 


Mica concentration 




Biotite gneiss 


Approximate contact 


Attitude of foliation 


Rim of open cut 




Survey point with altitude 

Mopped by EWmHeinnch ondRWLemke 9/25/44 

Fig. 6. — Map and Section of the Tilley Mine, Jackson County. 

The country rock is medium-grained biotite-garnet gneiss, the foliation of which strikes northeast and dips 
steeply southeast. The pegmatite is a tabular body which strikes north, dips moderately west, and averages 
about 4 feet in thickness. Closely associated with the pegmatite body are lenticular pods and tabular masses 
of fine-grained granite, composed of quartz, plagioclase, muscovite, and biotite. Bodies of granite occur between 
the pegmatite and the gneiss, and smaller pods of it also lie within the main pegmatite body. 

The pegmatite is a medium- to coarse-grained intergrowth of plagioclase, quartz, and muscovite. Biotite 
and garnet are common near the contacts with the gneiss. Pyrrhotite and apatite are common accessory min- 
erals in the granite. Pyrrhotite and a dark-green chlorite occur in gneiss along the contacts with the pegma- 
tite body. 

Coarse muscovite occurs along the contacts between pegmatite and granite and along contacts between 
pegmatite and gneiss. Mica books are locally so abundant in both of these zones that they constitute as much 
as 50 percent of the rock. The mica books have unusually well-developed crystal faces. The longest dimension 
of the crystals is commonly perpendicular to the cleavage. The largest book observed was 14 inches in di- 
ameter. The mica is unusually hard, generally flat, and of a very dark rum to greenish rum color. The chief 
defects are minute cracks and small quartz inclusions. Ruling is uncommon, but many of the books contain 
films of sulfides, both along the cleavage planes and around the edges. 

In September 1944 the southwestern corner of the stope exposed only barren granite ; the pegmatite had 
pinched out completely in this direction. However, pegmatite containing abundant small books of mica was 
exposed along the northwestern face of the stope. 


M. R. Klepper 

The Turkey Nest and Lyle Cut mines are on the south side of a high ridge about a mile east of Wayah 
Bald. The Turkey Nest mine (pi. 19) has been operated intermittently for the past nine years by J. L. Barnard 
of Franklin. In 1944, work was proceeding in the upper (west) drift. Information regarding the old work- 
ings in the eastern two-thirds of the area mapped is not available. According to Mr. Barnard these were 
probably mined forty or fifty years ago. 

The pegmatite at the Turkey Nest mine is enclosed in biotite gneiss which strikes from N.70°E. to east 
and dips 45-65°N. The pegmatite body strikes N.53°E., dips 45-60°S., and is about 7!/2 feet thick on the 
average. It is well zoned, consisting of a central tabular mass of quartz 3 to 5 feet thick flanked on each side 
by mica-bearing pegmatite 1.5 to 2.5 feet thick. The mica-bearing pegmatite is a medium- to coarse-grained 

Sylva District, North Carolina 




^ geology 

n. restored 





A SECTION A-A' •*■*■ 




Dump rock and muck 

Sheet-mica pegmatite 

Scrap-mica pegmatite 


Plogioclase-quartz pegmatite 

Biolite gneiss and hornblende gneiss 

Strike and dip of foliation 

Contact, observed, showing dip 

Contact, approximate 

Contact between pegmatite units 

Limit of exposure 

Outlines of underground workings' 
4724 -foot level 
4674 -foot level 
4600 -foot level 
Inaccessible stopes (reported) 
Accessible slope 


4&"^& . Rim of open cut 
_..--- ; Dump margin 

To* er 


(^■■4800 ft. 

Contour Interval 10 feet 
Datum assumed 

Geology and topography by 
M. R. Klepper ond L.C. Pray February 23-24, 1944 

Map and Sections of the Turkey Nest Mine, Macon County. 

aggregate of gray plagioclase (oligoclase?) quartz, and muscovite. Part of the muscovite occurs as small 
scrappy books intergrown with quartz and feldspar, and part as larger books distributed here and there 
throughout the zone. The new drift and stope expose only the part of the pegmatite body between the quartz 
core and the hanging-wall gneiss, which, according to Mr. Barnard, contains a higher concentration of mica 
than the footwall zone. The quality of the footwall mica, however, is reported to be somewhat the better. 
The mica is rum or ruby colored, and part of it has "A" structure. An estimated half is black specked. 

It seems likely that the Turkey Nest explores the same pegmatite body as the Lyle Cut mine, which lies 
about 500 feet to the southwest and is strikingly similar in structure and mineralogy. The Lyle Cut mine 

56 Mica Deposits of the Franklin- 

was first operated by Dr. J. M. Lyle about 1870. It was then operated intermittently and on a small scale by 
various operators until the end of World War I, .hen General Mica Company, of Baltimore, took over and op- 
erated for about three years. Philip S. Hoyt and Will McKinney each operated for a short time during 1941 and 
1942, and Gilmer Jones, a Franklin attorney, operated the mine from March to October 1943. It has been in- 
active since then. The pegmatite body has been developed by (1) a tabular open-cut and stope having a max- 
imum length of 225 feet, a maximum depth of 85 feet, and an average width of about 5 feet, (2) a 23-foot 
vertical shaft with a short drift at the bottom, (3) a 20-foot adit, and (4) a few shallow pits. 

The pegmatite at the Lyle Cut mine is a well-defined tabular body. It strikes N.50°E., dips 60° to 65°SE. 
and averages 4i/£ to 5 feet in thickness. The pegmatite body narrows to the southwest and is only 12 to 
14 inches thick in the pillar above the lower entry into the stope. It seems probable that the pegmatite pinches 
out within a hundred feet or less southwest of the entry. The maximum thickness measured between walls 
of the stope was 9 feet. 

Except in the entry pillar, the exposed pegmatite consists of a tabular quartz core, generally li/2 to 3 feet 
thick, sheathed by 1 to 2 y 2 feet of mica-bearing pegmatite. The quartz core has a distinctive streaky appear- 
ance that more or less parallels the walls of the pegmatite. Alternate bands are gray and milky, and a little 
feldspar has crystallized in some bands. The appearance suggests that the quartz may have been sheared 
parallel to the walls near the end of the period of crystallization. 

The pegmatite is a medium-to coarse-grained aggregate of milky to gray plagioclase (oligoclase?), quartz, 
and muscovite. Biotite occurs sparingly. One small black tourmaline crystal was found on the dump. The 
muscovite occurs as small, scrappy intergrowths with quartz and feldspar and as scattered books. In general 
the greater concentration of muscovite is reported to occur between the quartz core and the hanging wall of 
the pegmatite. 

The pegmatite has been intruded into fine- to medium-grained garnet-biotite gneiss, which strikes be- 
tween N.65°E. and east, and dips between 50° and 65°NW. White feldspar metacrysts accentuate the layer- 
ing of the gneiss. A little hornblende occurs in some layers.